- Articles & preprints
- Submission
- Policies
- Peer review
- Editorial board
- About
- EGU publications
- Manuscript tracking
Journal cover
Journal topic
Atmospheric Measurement Techniques
An interactive open-access journal of the European Geosciences Union
Journal topic
- Articles & preprints
- Submission
- Policies
- Peer review
- Editorial board
- About
- EGU publications
- Manuscript tracking
Journal metrics
IF3.668
IF 5-year
3.707
3.707
CiteScore
6.3
6.3
SNIP1.383
IPP3.75
SJR1.525
Scimago H
index77
index77
h5-index49
Abstracted/indexed
Abstracted/indexed
AMT | Articles | Volume 13, issue 10
Atmos. Meas. Tech., 13, 5303–5317, 2020
https://doi.org/10.5194/amt-13-5303-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/amt-13-5303-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Meas. Tech., 13, 5303–5317, 2020
https://doi.org/10.5194/amt-13-5303-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/amt-13-5303-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Research article 08 Oct 2020
Research article | 08 Oct 2020
Interannual and seasonal variations in the aerosol optical depth of the atmosphere in two regions of Spitsbergen (2002–2018)
Dmitry M. Kabanov et al.
Related authors
Tatiana B. Zhuravleva, Dmitriy M. Kabanov, Ilmir M. Nasrtdinov, Tatiana V. Russkova, Sergey M. Sakerin, Alexander Smirnov, and Brent N. Holben
Atmos. Meas. Tech., 10, 179–198, https://doi.org/10.5194/amt-10-179-2017, https://doi.org/10.5194/amt-10-179-2017, 2017
Short summary
Short summary
Aerosol properties were studied during a mega-fire event in summer 2012 over Siberia using ground-based measurements of spectral solar radiation at the AERONET site in Tomsk and satellite observations. The data were analysed using multi-year measurements under background conditions and yearly observed wildfires. It is shown that the aerosol radiation characteristics during individual severe fires differ significantly from the ensemble smoke hazes which are typical for the Siberian region.
S. M. Sakerin, A. A. Bobrikov, O. A. Bukin, L. P. Golobokova, Vas. V. Pol'kin, Vik. V. Pol'kin, K. A. Shmirko, D. M. Kabanov, T. V. Khodzher, N. A. Onischuk, A. N. Pavlov, V. L. Potemkin, and V. F. Radionov
Atmos. Chem. Phys., 15, 12413–12443, https://doi.org/10.5194/acp-15-12413-2015, https://doi.org/10.5194/acp-15-12413-2015, 2015
Short summary
Short summary
We discuss the spatiotemporal variations in aerosol characteristics, measured along the Northern Sea Route in RV Akademik Fedorov and RV Professor Khljustin cruises. The variability ranges of the average aerosol parameters in separate seas and regions were from 2.5 to 24cm-3 for number concentration of particles; from 830 to 2970ngm-3 for aerosol mass concentrations; from 20 to 150ngm-3 for black carbon mass concentrations; and from 0.03 to 0.19 for aerosol optical depth (0.5um).
G. G. Matvienko, B. D. Belan, M. V. Panchenko, O. A. Romanovskii, S. M. Sakerin, D. M. Kabanov, S. A. Turchinovich, Y. S. Turchinovich, T. A. Eremina, V. S. Kozlov, S. A. Terpugova, V. V. Pol'kin, E. P. Yausheva, D. G. Chernov, T. B. Zhuravleva, T. V. Bedareva, S. L. Odintsov, V. D. Burlakov, A. V. Nevzorov, M. Y. Arshinov, G. A. Ivlev, D. E. Savkin, A. V. Fofonov, V. A. Gladkikh, A. P. Kamardin, Y. S. Balin, G. P. Kokhanenko, I. E. Penner, S. V. Samoilova, P. N. Antokhin, V. G. Arshinova, D. K. Davydov, A. V. Kozlov, D. A. Pestunov, T. M. Rasskazchikova, D. V. Simonenkov, T. K. Sklyadneva, G. N. Tolmachev, S. B. Belan, V. P. Shmargunov, A. S. Kozlov, and S. B. Malyshkin
Atmos. Meas. Tech., 8, 4507–4520, https://doi.org/10.5194/amt-8-4507-2015, https://doi.org/10.5194/amt-8-4507-2015, 2015
Short summary
Short summary
The primary objective of the Complex Aerosol Experiment was measurement of microphysical, chemical, and optical properties of aerosol particles in the surface air layer and free atmosphere. The measurement data were used to retrieve the whole set of aerosol optical parameters, necessary for radiation calculations. Three measurement cycles were performed within the experiment during 2013: in spring, summer (July), and in late summer/early autumn.
Tatiana Nomokonova, Kerstin Ebell, Ulrich Löhnert, Marion Maturilli, and Christoph Ritter
Atmos. Chem. Phys., 20, 5157–5173, https://doi.org/10.5194/acp-20-5157-2020, https://doi.org/10.5194/acp-20-5157-2020, 2020
Short summary
Short summary
This paper presents an influence of water vapor anomalies on cloud properties and their radiative effect at Ny-Ålesund. The study is based on a 2.5-year active and passive cloud observation and a radiative transfer model. The results show that moist and dry conditions are related to strong changes in cloud occurrence, phase partitioning, water path, and, consequently, modulate the surface radiative budget.
Tatiana Nomokonova, Kerstin Ebell, Ulrich Löhnert, Marion Maturilli, Christoph Ritter, and Ewan O'Connor
Atmos. Chem. Phys., 19, 4105–4126, https://doi.org/10.5194/acp-19-4105-2019, https://doi.org/10.5194/acp-19-4105-2019, 2019
Short summary
Short summary
In this study, properties of clouds at the French–German Arctic research station in Ny-Ålesund are related to in-cloud thermodynamic conditions. The dataset used was collected within the Arctic Amplification project with a set of active and passive remote instruments. The results are compared with a model output. Significant divergence in observations and modelling of single-layer ice and mixed-phase clouds was found.
Justyna Lisok, Anna Rozwadowska, Jesper G. Pedersen, Krzysztof M. Markowicz, Christoph Ritter, Jacek W. Kaminski, Joanna Struzewska, Mauro Mazzola, Roberto Udisti, Silvia Becagli, and Izabela Gorecka
Atmos. Chem. Phys., 18, 8829–8848, https://doi.org/10.5194/acp-18-8829-2018, https://doi.org/10.5194/acp-18-8829-2018, 2018
Short summary
Short summary
The aim of the presented study was to investigate the impact on the radiation budget and atmospheric dynamics of a biomass-burning plume, transported from Alaska to the High Arctic region of Ny-Ålesund, Svalbard, in early July 2015. We found that the smoke plume may significantly alter radiative properties of the atmosphere. Furthermore, the simulations of atmospheric dynamics indicated a vertical positive displacement and broadening of the plume with time.
Tatiana B. Zhuravleva, Dmitriy M. Kabanov, Ilmir M. Nasrtdinov, Tatiana V. Russkova, Sergey M. Sakerin, Alexander Smirnov, and Brent N. Holben
Atmos. Meas. Tech., 10, 179–198, https://doi.org/10.5194/amt-10-179-2017, https://doi.org/10.5194/amt-10-179-2017, 2017
Short summary
Short summary
Aerosol properties were studied during a mega-fire event in summer 2012 over Siberia using ground-based measurements of spectral solar radiation at the AERONET site in Tomsk and satellite observations. The data were analysed using multi-year measurements under background conditions and yearly observed wildfires. It is shown that the aerosol radiation characteristics during individual severe fires differ significantly from the ensemble smoke hazes which are typical for the Siberian region.
Marion Maturilli and Christoph Ritter
Earth Syst. Sci. Data, 8, 159–164, https://doi.org/10.5194/essd-8-159-2016, https://doi.org/10.5194/essd-8-159-2016, 2016
Short summary
Short summary
The total solar eclipse over Ny-Ålesund (78.9° N, 11.9° E), Svalbard, on 20 March 2015 has been followed by various sensors. Here, we present the surface radiation measurements in the context of the meteorological observations, providing basic data for further studies on e.g. radiative transfer or micrometeorology.
S. M. Sakerin, A. A. Bobrikov, O. A. Bukin, L. P. Golobokova, Vas. V. Pol'kin, Vik. V. Pol'kin, K. A. Shmirko, D. M. Kabanov, T. V. Khodzher, N. A. Onischuk, A. N. Pavlov, V. L. Potemkin, and V. F. Radionov
Atmos. Chem. Phys., 15, 12413–12443, https://doi.org/10.5194/acp-15-12413-2015, https://doi.org/10.5194/acp-15-12413-2015, 2015
Short summary
Short summary
We discuss the spatiotemporal variations in aerosol characteristics, measured along the Northern Sea Route in RV Akademik Fedorov and RV Professor Khljustin cruises. The variability ranges of the average aerosol parameters in separate seas and regions were from 2.5 to 24cm-3 for number concentration of particles; from 830 to 2970ngm-3 for aerosol mass concentrations; from 20 to 150ngm-3 for black carbon mass concentrations; and from 0.03 to 0.19 for aerosol optical depth (0.5um).
G. G. Matvienko, B. D. Belan, M. V. Panchenko, O. A. Romanovskii, S. M. Sakerin, D. M. Kabanov, S. A. Turchinovich, Y. S. Turchinovich, T. A. Eremina, V. S. Kozlov, S. A. Terpugova, V. V. Pol'kin, E. P. Yausheva, D. G. Chernov, T. B. Zhuravleva, T. V. Bedareva, S. L. Odintsov, V. D. Burlakov, A. V. Nevzorov, M. Y. Arshinov, G. A. Ivlev, D. E. Savkin, A. V. Fofonov, V. A. Gladkikh, A. P. Kamardin, Y. S. Balin, G. P. Kokhanenko, I. E. Penner, S. V. Samoilova, P. N. Antokhin, V. G. Arshinova, D. K. Davydov, A. V. Kozlov, D. A. Pestunov, T. M. Rasskazchikova, D. V. Simonenkov, T. K. Sklyadneva, G. N. Tolmachev, S. B. Belan, V. P. Shmargunov, A. S. Kozlov, and S. B. Malyshkin
Atmos. Meas. Tech., 8, 4507–4520, https://doi.org/10.5194/amt-8-4507-2015, https://doi.org/10.5194/amt-8-4507-2015, 2015
Short summary
Short summary
The primary objective of the Complex Aerosol Experiment was measurement of microphysical, chemical, and optical properties of aerosol particles in the surface air layer and free atmosphere. The measurement data were used to retrieve the whole set of aerosol optical parameters, necessary for radiation calculations. Three measurement cycles were performed within the experiment during 2013: in spring, summer (July), and in late summer/early autumn.
Related subject area
Subject: Aerosols | Technique: Remote Sensing | Topic: Validation and Intercomparisons
Evaluation of UV aerosol retrievals from an ozone lidar
Aerosol data assimilation in the MOCAGE chemical transport model during the TRAQA/ChArMEx campaign: lidar observations
Application of low-cost fine particulate mass monitors to convert satellite aerosol optical depth to surface concentrations in North America and Africa
Evaluation of the OMPS/LP stratospheric aerosol extinction product using SAGE III/ISS observations
A fast visible-wavelength 3D radiative transfer model for numerical weather prediction visualization and forward modeling
A first comparison of TROPOMI aerosol layer height (ALH) to CALIOP data
Combining low-cost, surface-based aerosol monitors with size-resolved satellite data for air quality applications
The 2018 fire season in North America as seen by TROPOMI: aerosol layer height intercomparisons and evaluation of model-derived plume heights
Evaluation of satellite-based aerosol datasets and the CAMS reanalysis over the ocean utilizing shipborne reference observations
Aerosol and cloud top height information of Envisat MIPAS measurements
Assessment of urban aerosol pollution over the Moscow megacity by the MAIAC aerosol product
Aerosol retrievals from different polarimeters during the ACEPOL campaign using a common retrieval algorithm
A review and framework for the evaluation of pixel-level uncertainty estimates in satellite aerosol remote sensing
Analysis of global three-dimensional aerosol structure with spectral radiance matching
A comparative evaluation of Aura-OMI and SKYNET near-UV single-scattering albedo products
Aerosol measurements with a shipborne Sun–sky–lunar photometer and collocated multiwavelength Raman polarization lidar over the Atlantic Ocean
Intercomparison of aerosol volume size distributions derived from AERONET ground-based remote sensing and LARGE in situ aircraft profiles during the 2011–2014 DRAGON and DISCOVER-AQ experiments
Validation, comparison, and integration of GOCI, AHI, MODIS, MISR, and VIIRS aerosol optical depth over East Asia during the 2016 KORUS-AQ campaign
Aerosol optical depth comparison between GAW-PFR and AERONET-Cimel radiometers from long-term (2005–2015) 1 min synchronous measurements
Accuracy assessment of MODIS land aerosol optical thickness algorithms using AERONET measurements over North America
Investigations into the development of a satellite-based aerosol climate data record using ATSR-2, AATSR and AVHRR data over north-eastern China from 1987 to 2012
Stratospheric aerosol characteristics from space-borne observations: extinction coefficient and Ångström exponent
Retrieval of aerosol properties from ceilometer and photometer measurements: long-term evaluation with in situ data and statistical analysis at Montsec (southern Pyrenees)
Novel aerosol extinction coefficients and lidar ratios over the ocean from CALIPSO–CloudSat: evaluation and global statistics
Radiometric calibration of a non-imaging airborne spectrometer to measure the Greenland ice sheet surface
Aerosol optical depth retrievals in central Amazonia from a multi-filter rotating shadow-band radiometer calibrated on-site
Aerosol backscatter profiles from ceilometers: validation of water vapor correction in the framework of CeiLinEx2015
Aerosol optical properties derived from POLDER-3/PARASOL (2005–2013) over the western Mediterranean Sea – Part 1: Quality assessment with AERONET and in situ airborne observations
Exploring systematic offsets between aerosol products from the two MODIS sensors
Validation of MODIS 3 km land aerosol optical depth from NASA's EOS Terra and Aqua missions
Comparison of dust-layer heights from active and passive satellite sensors
Vertical profiles of aerosol mass concentration derived by unmanned airborne in situ and remote sensing instruments during dust events
Intercomparison of aerosol measurements performed with multi-wavelength Raman lidars, automatic lidars and ceilometers in the framework of INTERACT-II campaign
Comparison of aerosol optical depth from satellite (MODIS), sun photometer and broadband pyrheliometer ground-based observations in Cuba
Spatial distribution analysis of the OMI aerosol layer height: a pixel-by-pixel comparison to CALIOP observations
Characterization of smoke and dust episode over West Africa: comparison of MERRA-2 modeling with multiwavelength Mie–Raman lidar observations
Collocation mismatch uncertainties in satellite aerosol retrieval validation
Consistency of aerosols above clouds characterization from A-Train active and passive measurements
Mixing layer height as an indicator for urban air quality?
Dust impact on surface solar irradiance assessed with model simulations, satellite observations and ground-based measurements
Consistency of dimensional distributions and refractive indices of desert dust measured over Lampedusa with IASI radiances
Retrieval of ash properties from IASI measurements
MAX-DOAS retrieval of aerosol extinction properties in Madrid, Spain
Validating MODIS above-cloud aerosol optical depth retrieved from “color ratio” algorithm using direct measurements made by NASA's airborne AATS and 4STAR sensors
AerGOM, an improved algorithm for stratospheric aerosol extinction retrieval from GOMOS observations – Part 2: Intercomparisons
Comparison of aerosol properties retrieved using GARRLiC, LIRIC, and Raman algorithms applied to multi-wavelength lidar and sun/sky-photometer data
The role of cloud contamination, aerosol layer height and aerosol model in the assessment of the OMI near-UV retrievals over the ocean
GOCI Yonsei Aerosol Retrieval (YAER) algorithm and validation during the DRAGON-NE Asia 2012 campaign
EARLINET instrument intercomparison campaigns: overview on strategy and results
Development and validation of satellite-based estimates of surface visibility
Shi Kuang, Bo Wang, Michael J. Newchurch, Kevin Knupp, Paula Tucker, Edwin W. Eloranta, Joseph P. Garcia, Ilya Razenkov, John T. Sullivan, Timothy A. Berkoff, Guillaume Gronoff, Liqiao Lei, Christoph J. Senff, Andrew O. Langford, Thierry Leblanc, and Vijay Natraj
Atmos. Meas. Tech., 13, 5277–5292, https://doi.org/10.5194/amt-13-5277-2020, https://doi.org/10.5194/amt-13-5277-2020, 2020
Short summary
Short summary
Ozone lidar is a state-of-the-art remote-sensing instrument to measure atmospheric ozone concentrations with high spatiotemporal resolution. In this study, we show that an ozone lidar can also provide reliable aerosol measurements through intercomparison with colocated aerosol lidar observations.
Laaziz El Amraoui, Bojan Sič, Andrea Piacentini, Virginie Marécal, Nicolas Frebourg, and Jean-Luc Attié
Atmos. Meas. Tech., 13, 4645–4667, https://doi.org/10.5194/amt-13-4645-2020, https://doi.org/10.5194/amt-13-4645-2020, 2020
Short summary
Short summary
The aim of this paper is to present the assimilation of lidar observations from the CALIOP instrument onboard the CALIPSO satellite in the chemistry-transport model of Météo-France, MOCAGE. We presented the first results of the assimilation of the extinction coefficient observations of the CALIOP lidar instrument during the pre-ChArMEx-TRAQA field campaign. We evaluated the added value of the assimilation product to better document a desert dust transport event compared to the model free run.
Carl Malings, Daniel M. Westervelt, Aliaksei Hauryliuk, Albert A. Presto, Andrew Grieshop, Ashley Bittner, Matthias Beekmann, and R. Subramanian
Atmos. Meas. Tech., 13, 3873–3892, https://doi.org/10.5194/amt-13-3873-2020, https://doi.org/10.5194/amt-13-3873-2020, 2020
Short summary
Short summary
Most air quality information comes from accurate but expensive instruments. These can be supplemented by lower-cost sensors to increase the density of ground data and expand monitoring into less well-instrumented areas, like sub-Saharan Africa. In this paper, we look at how low-cost sensor data can be combined with satellite information on air quality (which requires ground data to properly calibrate measurements) and assess the benefits these low-cost sensors provide in this context.
Zhong Chen, Pawan K. Bhartia, Omar Torres, Glen Jaross, Robert Loughman, Matthew DeLand, Peter Colarco, Robert Damadeo, and Ghassan Taha
Atmos. Meas. Tech., 13, 3471–3485, https://doi.org/10.5194/amt-13-3471-2020, https://doi.org/10.5194/amt-13-3471-2020, 2020
Short summary
Short summary
The scope of the paper is the evaluation of stratospheric aerosols derived from the OMPS/LP instrument via comparison with independent datasets from the SAGE III/ISS instrument. Results show very good agreement for extinction profiles between an altitude of 19 and 27 km, to within ±25 %, and show systematic differences (LP-SAGE III/ISS) above 28 km and below 19 km (greater than ±25 %).
Steven Albers, Stephen M. Saleeby, Sonia Kreidenweis, Qijing Bian, Peng Xian, Zoltan Toth, Ravan Ahmadov, Eric James, and Steven D. Miller
Atmos. Meas. Tech., 13, 3235–3261, https://doi.org/10.5194/amt-13-3235-2020, https://doi.org/10.5194/amt-13-3235-2020, 2020
Short summary
Short summary
A fast 3D visible-light forward operator is used to realistically visualize, validate, and potentially assimilate ground- and space-based camera and satellite imagery with NWP models. Three-dimensional fields of hydrometeors, aerosols, and 2D land surface variables are considered in the generation of radiance fields and RGB imagery from a variety of vantage points.
Swadhin Nanda, Martin de Graaf, J. Pepijn Veefkind, Maarten Sneep, Mark ter Linden, Jiyunting Sun, and Pieternel F. Levelt
Atmos. Meas. Tech., 13, 3043–3059, https://doi.org/10.5194/amt-13-3043-2020, https://doi.org/10.5194/amt-13-3043-2020, 2020
Short summary
Short summary
This paper presents a first validation of the TROPOspheric Monitoring Instrument (TROPOMI) aerosol layer height (ALH) product, which is an estimate of the height of an aerosol layer using a spectrometer on board ESA's Sentinel-5 Precursor satellite mission. Comparison between the TROPOMI ALH product and co-located aerosol extinction heights from the CALIOP instrument on board NASA's CALIPSO mission show good agreement for selected cases over the ocean and large differences over land.
Priyanka deSouza, Ralph A. Kahn, James A. Limbacher, Eloise A. Marais, Fábio Duarte, and Carlo Ratti
Atmos. Meas. Tech. Discuss., https://doi.org/10.5194/amt-2020-136, https://doi.org/10.5194/amt-2020-136, 2020
Revised manuscript accepted for AMT
Short summary
Short summary
This paper presents a novel method to calibrate satellite data using low-cost optical particle counters (OPCs) to develop higher quality particulate matter (PM) estimates. This method could enable cities that do not have access to expensive reference air quality monitors, many of which are in the global South, to develop locally calibrated PM estimates from satellite data. Such information can be crucial for the development of effective air quality management plans.
Debora Griffin, Christopher Sioris, Jack Chen, Nolan Dickson, Andrew Kovachik, Martin de Graaf, Swadhin Nanda, Pepijn Veefkind, Enrico Dammers, Chris A. McLinden, Paul Makar, and Ayodeji Akingunola
Atmos. Meas. Tech., 13, 1427–1445, https://doi.org/10.5194/amt-13-1427-2020, https://doi.org/10.5194/amt-13-1427-2020, 2020
Short summary
Short summary
This study looks into validating the aerosol layer height product from the recently launched TROPOspheric Monitoring Instrument (TROPOMI) for forest fire plume through comparisons with two other satellite products, and interpreting differences due to the individual measurement techniques. These satellite observations are compared to predicted plume heights from Environment and Climate Change's air quality forecast model.
Jonas Witthuhn, Anja Hünerbein, and Hartwig Deneke
Atmos. Meas. Tech., 13, 1387–1412, https://doi.org/10.5194/amt-13-1387-2020, https://doi.org/10.5194/amt-13-1387-2020, 2020
Short summary
Short summary
Reliable reference measurements over ocean are essential for the evaluation and improvement of satellite- and model-based aerosol datasets. Here, a uniqe set of shipborne reference aerosol products obtained from Microtops sunphotometer and GUVis-3511 shadowband radiometer observations are compared to aerosol products from the MODIS and SEVIRI satellite sensors, and the CAMS reanalysis over the Atlantic Ocean. The present evaluation highlights the importance of an aerosol-type based analysis.
Sabine Griessbach, Lars Hoffmann, Reinhold Spang, Peggy Achtert, Marc von Hobe, Nina Mateshvili, Rolf Müller, Martin Riese, Christian Rolf, Patric Seifert, and Jean-Paul Vernier
Atmos. Meas. Tech., 13, 1243–1271, https://doi.org/10.5194/amt-13-1243-2020, https://doi.org/10.5194/amt-13-1243-2020, 2020
Short summary
Short summary
In this paper we study the cloud top height derived from MIPAS measurements. Previous studies showed contradictory results with respect to MIPAS, both underestimating and overestimating cloud top height. We used simulations and found that overestimation and/or underestimation depend on cloud extinction. To support our findings we compared MIPAS cloud top heights of volcanic sulfate aerosol with measurements from CALIOP, ground-based lidar, and ground-based twilight measurements.
Ekaterina Y. Zhdanova, Natalia Y. Chubarova, and Alexei I. Lyapustin
Atmos. Meas. Tech., 13, 877–891, https://doi.org/10.5194/amt-13-877-2020, https://doi.org/10.5194/amt-13-877-2020, 2020
Short summary
Short summary
We estimated the distribution of aerosol optical thickness (AOT) with a spatial resolution of 1 km over the Moscow megacity using the MAIAC satellite aerosol product from May to September over the years 2000–2017. We revealed that the MAIAC product is a reliable instrument for assessing the spatial features of urban aerosol pollution and its temporal dynamics. The local aerosol effect is about 0.02–0.04 in AOT in the visible spectral range over the Moscow megacity.
Guangliang Fu, Otto Hasekamp, Jeroen Rietjens, Martijn Smit, Antonio Di Noia, Brian Cairns, Andrzej Wasilewski, David Diner, Felix Seidel, Feng Xu, Kirk Knobelspiesse, Meng Gao, Arlindo da Silva, Sharon Burton, Chris Hostetler, John Hair, and Richard Ferrare
Atmos. Meas. Tech., 13, 553–573, https://doi.org/10.5194/amt-13-553-2020, https://doi.org/10.5194/amt-13-553-2020, 2020
Short summary
Short summary
In this paper, we present aerosol retrieval results from the ACEPOL (Aerosol Characterization from Polarimeter and Lidar) campaign, which was a joint initiative between NASA and SRON (the Netherlands Institute for Space Research). We perform aerosol retrievals from different multi-angle polarimeters employed during the ACEPOL campaign and evaluate them against ground-based AERONET measurements and High Spectral Resolution Lidar-2 (HSRL-2) measurements.
Andrew M. Sayer, Yves Govaerts, Pekka Kolmonen, Antti Lipponen, Marta Luffarelli, Tero Mielonen, Falguni Patadia, Thomas Popp, Adam C. Povey, Kerstin Stebel, and Marcin L. Witek
Atmos. Meas. Tech., 13, 373–404, https://doi.org/10.5194/amt-13-373-2020, https://doi.org/10.5194/amt-13-373-2020, 2020
Short summary
Short summary
Satellite measurements of the Earth are routinely processed to estimate useful quantities; one example is the amount of atmospheric aerosols (which are particles such as mineral dust, smoke, volcanic ash, or sea spray). As with all measurements and inferred quantities, there is some degree of uncertainty in this process.
There are various methods to estimate these uncertainties. A related question is the following: how reliable are these estimates? This paper presents a method to assess them.
Dong Liu, Sijie Chen, Chonghui Cheng, Howard W. Barker, Changzhe Dong, Ju Ke, Shuaibo Wang, and Zhuofan Zheng
Atmos. Meas. Tech., 12, 6541–6556, https://doi.org/10.5194/amt-12-6541-2019, https://doi.org/10.5194/amt-12-6541-2019, 2019
Short summary
Short summary
Aerosols are one of the drivers of climate change, and more information about aerosol vertical distribution is needed to analyze the role of aerosols in the atmosphere. In this work, we match and substitute a pixel along the lidar ground track for every pixel that is not on the track based on the radiance measured by a passive imager, therefore expanding the atmosphere profiles to a nearby region. The accuracy of the construction is confirmed through a procedure mimicking the construction.
Hiren Jethva and Omar Torres
Atmos. Meas. Tech., 12, 6489–6503, https://doi.org/10.5194/amt-12-6489-2019, https://doi.org/10.5194/amt-12-6489-2019, 2019
Short summary
Short summary
The intercomparison of satellite- and ground-measured aerosol absorption properties, such as presented here using Aura-OMI and SKYNET sensors, constitutes an important exercise to evaluate relative performance, track algorithm changes, and to diagnose retrieval accuracy and issues. The two datasets are found to agree reasonably well under moderate to higher aerosol loading but show disagreement under lower aerosol amounts due to retrieval issues in both techniques.
Zhenping Yin, Albert Ansmann, Holger Baars, Patric Seifert, Ronny Engelmann, Martin Radenz, Cristofer Jimenez, Alina Herzog, Kevin Ohneiser, Karsten Hanbuch, Luc Blarel, Philippe Goloub, Gaël Dubois, Stephane Victori, and Fabrice Maupin
Atmos. Meas. Tech., 12, 5685–5698, https://doi.org/10.5194/amt-12-5685-2019, https://doi.org/10.5194/amt-12-5685-2019, 2019
Short summary
Short summary
A new shipborne Sun–sky–lunar photometer was validated through comparisons with collocated MICROTOPS II and multiwavelength Raman polarization lidar measurements during two trans-Atlantic cruises. A full diurnal cycle of mixed dust–smoke episode was captured by both the shipborne photometer and lidar. The coefficient of determination for the linear regression between MICROTOPS II and the shipborne photometer was 0.993 for AOD at 500 nm based on the entire dataset.
Joel S. Schafer, Tom F. Eck, Brent N. Holben, Kenneth L. Thornhill, Luke D. Ziemba, Patricia Sawamura, Richard H. Moore, Ilya Slutsker, Bruce E. Anderson, Alexander Sinyuk, David M. Giles, Alexander Smirnov, Andreas J. Beyersdorf, and Edward L. Winstead
Atmos. Meas. Tech., 12, 5289–5301, https://doi.org/10.5194/amt-12-5289-2019, https://doi.org/10.5194/amt-12-5289-2019, 2019
Short summary
Short summary
Two independent datasets of column-integrated size distributions of atmospheric aerosols were compared during four 1-month regional campaigns from 2011 to 2014 in four US states. One set of measurements was from observations at multiple locations at the surface using retrievals from sun photometers, while the other relied on in situ aircraft sampling. These campaigns represent the most extensive comparison of AERONET size distributions with aircraft sampling of particle size on record.
Myungje Choi, Hyunkwang Lim, Jhoon Kim, Seoyoung Lee, Thomas F. Eck, Brent N. Holben, Michael J. Garay, Edward J. Hyer, Pablo E. Saide, and Hongqing Liu
Atmos. Meas. Tech., 12, 4619–4641, https://doi.org/10.5194/amt-12-4619-2019, https://doi.org/10.5194/amt-12-4619-2019, 2019
Short summary
Short summary
Satellite-based aerosol optical depth (AOD) products have been improved continuously and available from multiple low Earth orbit sensors, such as MODIS, MISR, and VIIRS, and geostationary sensors, such as GOCI and AHI, over East Asia. These multi-satellite AOD products are validated, intercompared, analyzed, and integrated to understand different characteristics, such as quality and spatio-temporal coverage, focused on several aerosol transportation cases during the 2016 KORUS-AQ campaign.
Emilio Cuevas, Pedro Miguel Romero-Campos, Natalia Kouremeti, Stelios Kazadzis, Petri Räisänen, Rosa Delia García, Africa Barreto, Carmen Guirado-Fuentes, Ramón Ramos, Carlos Toledano, Fernando Almansa, and Julian Gröbner
Atmos. Meas. Tech., 12, 4309–4337, https://doi.org/10.5194/amt-12-4309-2019, https://doi.org/10.5194/amt-12-4309-2019, 2019
Short summary
Short summary
A comprehensive comparison of more than 70 000 synchronous 1 min aerosol optical depth (AOD) data from 3 Global Atmosphere Watch precision filter radiometers (GAW-PFR) and 15 Aerosol Robotic Network Cimel radiometers (AERONET-Cimel) was performed for the four
nearwavelengths (380, 440, 500 and 870 nm) in the period 2005–2015. The goal of this study is to assess whether their long term AOD data are comparable and consistent.
Hiren Jethva, Omar Torres, and Yasuko Yoshida
Atmos. Meas. Tech., 12, 4291–4307, https://doi.org/10.5194/amt-12-4291-2019, https://doi.org/10.5194/amt-12-4291-2019, 2019
Short summary
Short summary
Accuracy assessment of the satellite-retrieved aerosol properties is an important exercise to validate and track the changes in the retrieval algorithm. Here, for the first time, three standard aerosol products derived from MODIS Aqua are compared against the ground-based AERONET dataset over the North American region. The present validation analysis provides guidance in the development of inversion schemes to derive aerosol properties from existing and future MODIS-like sensors.
Yahui Che, Jie Guang, Gerrit de Leeuw, Yong Xue, Ling Sun, and Huizheng Che
Atmos. Meas. Tech., 12, 4091–4112, https://doi.org/10.5194/amt-12-4091-2019, https://doi.org/10.5194/amt-12-4091-2019, 2019
Short summary
Short summary
The use of AOD data retrieved from ATSR-2, AATSR and AVHRR to produce a very long time series is investigated. The study is made over a small area in northern China with a large variation of AOD values. Sun photometer data from AERONET and CARSNET and radiance-derived AOD are used as reference. The results show that all data sets compare well. However, AVHRR underestimates high AOD (mainly occurring in summer) but performs better than (A)ATSR in winter.
Elizaveta Malinina, Alexei Rozanov, Landon Rieger, Adam Bourassa, Heinrich Bovensmann, John P. Burrows, and Doug Degenstein
Atmos. Meas. Tech., 12, 3485–3502, https://doi.org/10.5194/amt-12-3485-2019, https://doi.org/10.5194/amt-12-3485-2019, 2019
Short summary
Short summary
This paper covers the problems related to the derivation of aerosol extinction coefficients and Ångström exponents from space-borne instruments working in limb and occultation viewing geometries. Aerosol extinction coefficients and Ångström exponents were calculated from the SCIAMACHY aerosol particle size data set. The results were compared with the data from SAGE II and OSIRIS. The Ångström exponent in the tropical regions and its dependency on particle size parameters are discussed.
Gloria Titos, Marina Ealo, Roberto Román, Alberto Cazorla, Yolanda Sola, Oleg Dubovik, Andrés Alastuey, and Marco Pandolfi
Atmos. Meas. Tech., 12, 3255–3267, https://doi.org/10.5194/amt-12-3255-2019, https://doi.org/10.5194/amt-12-3255-2019, 2019
Short summary
Short summary
We present new results of vertically resolved extensive aerosol optical properties (backscattering, scattering and extinction) and volume concentrations retrieved with the GRASP algorithm from ceilometer and photometer measurements. Long-term evaluation with in situ data gathered at the Montsec mountaintop observatory (northeastern Spain) shows good agreement, being a step forward towards a better representation of aerosol vertical distribution with wide spatial coverage.
David Painemal, Marian Clayton, Richard Ferrare, Sharon Burton, Damien Josset, and Mark Vaughan
Atmos. Meas. Tech., 12, 2201–2217, https://doi.org/10.5194/amt-12-2201-2019, https://doi.org/10.5194/amt-12-2201-2019, 2019
Short summary
Short summary
We present 1 year of a new CALIOP-based aerosol extinction coefficient and lidar ratio over the ocean, with the goal of providing a flexible dataset for climate research as well as independent retrievals that can be helpful for refining CALIPSO Science Team algorithms. The retrievals are derived by constraining the lidar equation with an aerosol optical depth estimated from cross-calibrated CALIOP and CloudSat surface echos.
Christopher J. Crawford, Jeannette van den Bosch, Kelly M. Brunt, Milton G. Hom, John W. Cooper, David J. Harding, James J. Butler, Philip W. Dabney, Thomas A. Neumann, Craig S. Cleckner, and Thorsten Markus
Atmos. Meas. Tech., 12, 1913–1933, https://doi.org/10.5194/amt-12-1913-2019, https://doi.org/10.5194/amt-12-1913-2019, 2019
Short summary
Short summary
This paper presents laboratory and in-flight radiometric methods to calibrate and deploy a full-spectrum non-imaging airborne visible-to-shortwave infrared (VSWIR) spectrometer to measure polar ice sheet surface optical properties. Using an atmospheric radiative transfer model and coincident Landsat 8 multispectral image, this study concluded that it is possible to measure bright Greenland ice and dark bare rock/soil targets at an airborne remote sensing uncertainty of between 0.6 and 4.7.
Nilton E. Rosário, Thamara Sauini, Theotonio Pauliquevis, Henrique M. J. Barbosa, Marcia A. Yamasoe, and Boris Barja
Atmos. Meas. Tech., 12, 921–934, https://doi.org/10.5194/amt-12-921-2019, https://doi.org/10.5194/amt-12-921-2019, 2019
Short summary
Short summary
Does pristine Amazonian forest atmosphere provide successful calibration of a Sun photometer based on the Langley plot method? This question emerged from the challenge of maintaining regular calibration of a Sun photometer dedicated to long-term monitoring of aerosol optical properties in Amazonia, far from clean mountaintops. Our results show that on-site calibrated Sun photometers, under pristine Amazonian conditions, are able to provide consistent retrieval of aerosol optical depth.
Matthias Wiegner, Ina Mattis, Margit Pattantyús-Ábrahám, Juan Antonio Bravo-Aranda, Yann Poltera, Alexander Haefele, Maxime Hervo, Ulrich Görsdorf, Ronny Leinweber, Josef Gasteiger, Martial Haeffelin, Frank Wagner, Jan Cermak, Katerina Komínková, Mike Brettle, Christoph Münkel, and Kornelia Pönitz
Atmos. Meas. Tech., 12, 471–490, https://doi.org/10.5194/amt-12-471-2019, https://doi.org/10.5194/amt-12-471-2019, 2019
Short summary
Short summary
Many ceilometers are influenced by water vapor absorption in the spectral range around 910 nm. Thus, a correction is required to retrieve aerosol optical properties. Validation of this correction scheme was performed in the framework of CeiLinEx2015 for several ceilometers with good agreement for Vaisala's CL51 ceilometer. For future applications we recommend monitoring the emitted wavelength and providing
darkmeasurements on a regular basis to be able to correct for signal artifacts.
Paola Formenti, Lydie Mbemba Kabuiku, Isabelle Chiapello, Fabrice Ducos, François Dulac, and Didier Tanré
Atmos. Meas. Tech., 11, 6761–6784, https://doi.org/10.5194/amt-11-6761-2018, https://doi.org/10.5194/amt-11-6761-2018, 2018
Short summary
Short summary
Aerosol particles from natural and anthropogenic sources are climate regulators as they can counteract or amplify the warming effect of greenhouse gases, but are difficult to observe due to their temporal and spatial variability. Satellite sensors can provide the needed global coverage but need validation. In this paper we explore the capability of the POLDER-3 advanced space-borne sensor to observe aerosols over the western Mediterranean region.
Robert C. Levy, Shana Mattoo, Virginia Sawyer, Yingxi Shi, Peter R. Colarco, Alexei I. Lyapustin, Yujie Wang, and Lorraine A. Remer
Atmos. Meas. Tech., 11, 4073–4092, https://doi.org/10.5194/amt-11-4073-2018, https://doi.org/10.5194/amt-11-4073-2018, 2018
Short summary
Short summary
Global aerosol data sets are essential for assessing climate-related questions. When comparing data sets derived from twin satellite sensors, we find consistent global offsets between morning and afternoon observations. Applying satellite-like sampling to a global model derives much weaker morning/afternoon offsets, suggesting that the observational differences are due to calibration. However, applying additional calibration corrections appears to reduce (but not remove) the global offsets.
Pawan Gupta, Lorraine A. Remer, Robert C. Levy, and Shana Mattoo
Atmos. Meas. Tech., 11, 3145–3159, https://doi.org/10.5194/amt-11-3145-2018, https://doi.org/10.5194/amt-11-3145-2018, 2018
Short summary
Short summary
In this study, we perform global validation of MODIS high-resolution (3 km) AOD over global land by comparing against AERONET measurements. The MODIS–AERONET collocated data sets consist of 161 410 high-confidence AOD pairs from 2000 to 2015 for Terra MODIS and 2003 to 2015 for Aqua MODIS. We find that 62.5 and 68.4 % of AODs retrieved from Terra MODIS and Aqua MODIS, respectively, fall within previously published expected error.
Arve Kylling, Sophie Vandenbussche, Virginie Capelle, Juan Cuesta, Lars Klüser, Luca Lelli, Thomas Popp, Kerstin Stebel, and Pepijn Veefkind
Atmos. Meas. Tech., 11, 2911–2936, https://doi.org/10.5194/amt-11-2911-2018, https://doi.org/10.5194/amt-11-2911-2018, 2018
Short summary
Short summary
The aerosol layer height is one of four aerosol parameters which is needed to enhance our understanding of aerosols' role in the climate system. Both active and passive measurement methods may be used to estimate the aerosol layer height. Aerosol height estimates made from passive infrared and solar satellite sensors measurements are compared with satellite-borne lidar estimates. There is considerable variation between the retrieved dust heights and how they compare with the lidar.
Dimitra Mamali, Eleni Marinou, Jean Sciare, Michael Pikridas, Panagiotis Kokkalis, Michael Kottas, Ioannis Binietoglou, Alexandra Tsekeri, Christos Keleshis, Ronny Engelmann, Holger Baars, Albert Ansmann, Vassilis Amiridis, Herman Russchenberg, and George Biskos
Atmos. Meas. Tech., 11, 2897–2910, https://doi.org/10.5194/amt-11-2897-2018, https://doi.org/10.5194/amt-11-2897-2018, 2018
Short summary
Short summary
The paper's scope is to evaluate the performance of in situ atmospheric aerosol instrumentation on board unmanned aerial vehicles (UAVs) and the performance of algorithms used to calculate the aerosol mass from remote sensing instruments by comparing the two independent techniques to each other. Our results indicate that UAV-based aerosol measurements (using specific in situ and remote sensing instrumentation) can provide reliable ways to determine the aerosol mass throughout the atmosphere.
Fabio Madonna, Marco Rosoldi, Simone Lolli, Francesco Amato, Joshua Vande Hey, Ranvir Dhillon, Yunhui Zheng, Mike Brettle, and Gelsomina Pappalardo
Atmos. Meas. Tech., 11, 2459–2475, https://doi.org/10.5194/amt-11-2459-2018, https://doi.org/10.5194/amt-11-2459-2018, 2018
Short summary
Short summary
The accurate monitoring of climate based on the use of low-cost and low-maintenance automatic system represents one of the challenges for the scientific community and instrument manufacturers for the next decade. In the frame of two experiments, INTERACT and INTERACT-II, taking place at CIAO (CNR-IMAA Atmospheric Observatory) in Tito Scalo, Potenza, Italy, commercial low-cost lidars have been compared with advanced lidar systems to assess their performances.
Juan Carlos Antuña-Marrero, Victoria Cachorro Revilla, Frank García Parrado, Ángel de Frutos Baraja, Albeth Rodríguez Vega, David Mateos, René Estevan Arredondo, and Carlos Toledano
Atmos. Meas. Tech., 11, 2279–2293, https://doi.org/10.5194/amt-11-2279-2018, https://doi.org/10.5194/amt-11-2279-2018, 2018
Short summary
Short summary
Comparing AOD measurements from MODIS (Terra and Aqua), sun photometer and pyrheliometers broadband instruments in Cuba.
Julien Chimot, J. Pepijn Veefkind, Tim Vlemmix, and Pieternel F. Levelt
Atmos. Meas. Tech., 11, 2257–2277, https://doi.org/10.5194/amt-11-2257-2018, https://doi.org/10.5194/amt-11-2257-2018, 2018
Short summary
Short summary
Aerosol layer height (ALH) was retrieved from the OMI 477 nm O2–O2 band and its spatial pattern evaluated over selected cloud-free scenes. We used a neural network approach previously trained and developed. Comparison with CALIOP aerosol level 2 products over urban and industrial pollution in east China shows consistent spatial patterns. In addition, we show the possibility to determine the height of thick aerosol layers released by intensive biomass burning events in South America and Russia.
Igor Veselovskii, Philippe Goloub, Thierry Podvin, Didier Tanre, Arlindo da Silva, Peter Colarco, Patricia Castellanos, Mikhail Korenskiy, Qiaoyun Hu, David N. Whiteman, Daniel Pérez-Ramírez, Patrick Augustin, Marc Fourmentin, and Alexei Kolgotin
Atmos. Meas. Tech., 11, 949–969, https://doi.org/10.5194/amt-11-949-2018, https://doi.org/10.5194/amt-11-949-2018, 2018
Short summary
Short summary
Observations of multiwavelength Mie–Raman lidar during smoke episode over West Africa are compared with the vertical distribution of aerosol parameters provided by the MERRA-2 model. The values of modeled and observed extinctions at both 355 nm and 532 nm are also rather close. The model predicts significant concentration of dust particles inside the smoke layer. This is supported by a high depolarization ratio of 15 % observed in the center of this layer.
Timo H. Virtanen, Pekka Kolmonen, Larisa Sogacheva, Edith Rodríguez, Giulia Saponaro, and Gerrit de Leeuw
Atmos. Meas. Tech., 11, 925–938, https://doi.org/10.5194/amt-11-925-2018, https://doi.org/10.5194/amt-11-925-2018, 2018
Short summary
Short summary
We study the collocation mismatch uncertainty related to validating coarse-resolution satellite-based aerosol data against point-like ground based measurements. We use the spatial variability in the satellite data to estimate the upper limit for the uncertainty and study the effect of sampling parameters in the validation. We find that accounting for the collocation mismatch uncertainty increases the fraction of consistent data in the validation.
Lucia T. Deaconu, Fabien Waquet, Damien Josset, Nicolas Ferlay, Fanny Peers, François Thieuleux, Fabrice Ducos, Nicolas Pascal, Didier Tanré, Jacques Pelon, and Philippe Goloub
Atmos. Meas. Tech., 10, 3499–3523, https://doi.org/10.5194/amt-10-3499-2017, https://doi.org/10.5194/amt-10-3499-2017, 2017
Short summary
Short summary
This study presents a comparison between active (CALIOP) and passive (POLDER) remote sensing methods, developed for retrieving aerosol above-cloud optical and microphysical properties. Main results show a good agreement when the aerosol microphysics is dominated by fine-mode particles or coarse-mode dust or when the aerosol layer is well separated from the cloud below. The paper is also focused on understanding the differences between the retrievals and the limitations of each method.
Alexander Geiß, Matthias Wiegner, Boris Bonn, Klaus Schäfer, Renate Forkel, Erika von Schneidemesser, Christoph Münkel, Ka Lok Chan, and Rainer Nothard
Atmos. Meas. Tech., 10, 2969–2988, https://doi.org/10.5194/amt-10-2969-2017, https://doi.org/10.5194/amt-10-2969-2017, 2017
Short summary
Short summary
Based on measurements with a ceilometer and from an air quality network, the relationship between the mixing layer height (MLH) and near surface concentrations of pollutants was investigated for summer 2014 in Berlin. It was found that the heterogeneity of the concentrations exceeds the differences due to different MLH retrievals. In particular for PM10 it seems to be unrealistic to find correlations between MLH and concentrations representative for an entire metropolitan area in flat terrain.
Panagiotis G. Kosmopoulos, Stelios Kazadzis, Michael Taylor, Eleni Athanasopoulou, Orestis Speyer, Panagiotis I. Raptis, Eleni Marinou, Emmanouil Proestakis, Stavros Solomos, Evangelos Gerasopoulos, Vassilis Amiridis, Alkiviadis Bais, and Charalabos Kontoes
Atmos. Meas. Tech., 10, 2435–2453, https://doi.org/10.5194/amt-10-2435-2017, https://doi.org/10.5194/amt-10-2435-2017, 2017
Short summary
Short summary
We study the impact of dust on solar energy using remote sensing data in conjunction with synergistic modelling and forecasting techniques. Under high aerosol loads, we found great solar energy losses of the order of 80 and 50% for concentrated solar power and photovoltaic installations, respectively. The 1-day forecast presented an overall accuracy within 10% in direct comparison to the real conditions under high energy potential, optimising the efficient energy planning and policies.
Giuliano Liuzzi, Guido Masiello, Carmine Serio, Daniela Meloni, Claudia Di Biagio, and Paola Formenti
Atmos. Meas. Tech., 10, 599–615, https://doi.org/10.5194/amt-10-599-2017, https://doi.org/10.5194/amt-10-599-2017, 2017
Short summary
Short summary
In this work we have given a contribution to better understand some of the properties of the desert dust plumes in the western Mediterranean, using both direct measurements and satellite observations. This study has mainly evidenced that satellite observations can provide information about the geographical provenance of dust. This is important because such variability is reflected in the way in which dust interacts with atmosphere and impacts over the observed infrared radiation from satellites.
Lucy J. Ventress, Gregory McGarragh, Elisa Carboni, Andrew J. Smith, and Roy G. Grainger
Atmos. Meas. Tech., 9, 5407–5422, https://doi.org/10.5194/amt-9-5407-2016, https://doi.org/10.5194/amt-9-5407-2016, 2016
Short summary
Short summary
The detection of volcanic ash plumes and knowledge of their properties have been of increasing interest due to the effect ash particles can have on the aviation industry. A new method is shown for use with hyperspectral satellite instruments, such as the Infrared Atmospheric Sounding Interferometer, to derive optical and physical properties of volcanic ash. The results are compared to ancillary data sources, showing good agreement, which indicates better characterisation of volcanic plumes.
Shanshan Wang, Carlos A. Cuevas, Udo Frieß, and Alfonso Saiz-Lopez
Atmos. Meas. Tech., 9, 5089–5101, https://doi.org/10.5194/amt-9-5089-2016, https://doi.org/10.5194/amt-9-5089-2016, 2016
Short summary
Short summary
Multi-axis differential optical absorption spectroscopy (MAX-DOAS) measurements were performed in the urban environment of Madrid, Spain, where Sahara dust intrusion sometimes occurs. The study shows a high performances in the retrieval of aerosol optical depth, the surface extinction coefficient and an elevated layer during dust episodes, validated by AERONET in situ and modeling data. It is essential to capture the extinction properties of both local aerosol and Saharan dust.
Hiren Jethva, Omar Torres, Lorraine Remer, Jens Redemann, John Livingston, Stephen Dunagan, Yohei Shinozuka, Meloe Kacenelenbogen, Michal Segal Rosenheimer, and Rob Spurr
Atmos. Meas. Tech., 9, 5053–5062, https://doi.org/10.5194/amt-9-5053-2016, https://doi.org/10.5194/amt-9-5053-2016, 2016
Short summary
Short summary
Validation of the above-cloud aerosol optical depth retrieved using the "color ratio" method applied to MODIS cloudy-sky
measurements against airborne direct measurements made by NASA’s AATS and 4STAR sun photometers during SAFARI-2000,
ACE-ASIA 2001, and SEAC4RS 2013 reveals a good level of agreement (difference < 0.1), in which most matchups are found
be constrained within the estimated uncertainties associated with the MODIS retrievals (-10 % to +50 %).
Charles Étienne Robert, Christine Bingen, Filip Vanhellemont, Nina Mateshvili, Emmanuel Dekemper, Cédric Tétard, Didier Fussen, Adam Bourassa, and Claus Zehner
Atmos. Meas. Tech., 9, 4701–4718, https://doi.org/10.5194/amt-9-4701-2016, https://doi.org/10.5194/amt-9-4701-2016, 2016
Short summary
Short summary
We compare stratospheric aerosol loading computed with a new computer algorithm with various established datasets to determine the overall agreement. Since the new results are based on observation of starlight through the Earth's atmosphere, various aspects of these measurements can influence the final results. A systematic analysis of these aspects, such as the star brightness and temperature, is carried out to see if, and how, they influence the agreement of the results with other datasets.
Valentyn Bovchaliuk, Philippe Goloub, Thierry Podvin, Igor Veselovskii, Didier Tanre, Anatoli Chaikovsky, Oleg Dubovik, Augustin Mortier, Anton Lopatin, Mikhail Korenskiy, and Stephane Victori
Atmos. Meas. Tech., 9, 3391–3405, https://doi.org/10.5194/amt-9-3391-2016, https://doi.org/10.5194/amt-9-3391-2016, 2016
Santiago Gassó and Omar Torres
Atmos. Meas. Tech., 9, 3031–3052, https://doi.org/10.5194/amt-9-3031-2016, https://doi.org/10.5194/amt-9-3031-2016, 2016
Short summary
Short summary
Aerosol optical depths derived by the OMI near-UV algorithm are evaluated against independent observations over the ocean. The comparison resulted in differences within the expected levels of uncertainty. In addition, in clear sky conditions, the retrieved AODs compare well with independent measurements but they are biased high in partially cloud-contaminated pixels. Additional sources of discrepancies are documented and will be corrected in future versions of the algorithm.
Myungje Choi, Jhoon Kim, Jaehwa Lee, Mijin Kim, Young-Je Park, Ukkyo Jeong, Woogyung Kim, Hyunkee Hong, Brent Holben, Thomas F. Eck, Chul H. Song, Jae-Hyun Lim, and Chang-Keun Song
Atmos. Meas. Tech., 9, 1377–1398, https://doi.org/10.5194/amt-9-1377-2016, https://doi.org/10.5194/amt-9-1377-2016, 2016
Short summary
Short summary
The Geostationary Ocean Color Imager (GOCI) is the first ocean color sensor in geostationary orbit. It enables hourly aerosol optical properties to be observed in high spatial resolution. This study presents improvements of the GOCI Yonsei Aerosol Retrieval (YAER) algorithm and its validation results using ground-based and other satellite-based observation products during DRAGON-NE Asia 2012 Campaign. Retrieval errors are also analyzed according to various factors through the validation studies.
Ulla Wandinger, Volker Freudenthaler, Holger Baars, Aldo Amodeo, Ronny Engelmann, Ina Mattis, Silke Groß, Gelsomina Pappalardo, Aldo Giunta, Giuseppe D'Amico, Anatoli Chaikovsky, Fiodor Osipenko, Alexander Slesar, Doina Nicolae, Livio Belegante, Camelia Talianu, Ilya Serikov, Holger Linné, Friedhelm Jansen, Arnoud Apituley, Keith M. Wilson, Martin de Graaf, Thomas Trickl, Helmut Giehl, Mariana Adam, Adolfo Comerón, Constantino Muñoz-Porcar, Francesc Rocadenbosch, Michaël Sicard, Sergio Tomás, Diego Lange, Dhiraj Kumar, Manuel Pujadas, Francisco Molero, Alfonso J. Fernández, Lucas Alados-Arboledas, Juan Antonio Bravo-Aranda, Francisco Navas-Guzmán, Juan Luis Guerrero-Rascado, María José Granados-Muñoz, Jana Preißler, Frank Wagner, Michael Gausa, Ivan Grigorov, Dimitar Stoyanov, Marco Iarlori, Vincenco Rizi, Nicola Spinelli, Antonella Boselli, Xuan Wang, Teresa Lo Feudo, Maria Rita Perrone, Ferdinando De Tomasi, and Pasquale Burlizzi
Atmos. Meas. Tech., 9, 1001–1023, https://doi.org/10.5194/amt-9-1001-2016, https://doi.org/10.5194/amt-9-1001-2016, 2016
Short summary
Short summary
We introduce the quality-assurance efforts of the European Aerosol Research Lidar Network (EARLINET) at instrument level. Within several campaigns, 21 EARLINET systems from 18 EARLINET stations were intercompared. A comprehensive strategy for campaign setup and data evaluation was established. The intercomparisons have reinforced our confidence in the EARLINET data quality and allowed us to draw conclusions on necessary system improvements and to identify major challenges for our future work.
J. Brunner, R. B. Pierce, and A. Lenzen
Atmos. Meas. Tech., 9, 409–422, https://doi.org/10.5194/amt-9-409-2016, https://doi.org/10.5194/amt-9-409-2016, 2016
Short summary
Short summary
A satellite based surface visibility retrieval has been developed for the GOES-R ABI instrument using MODIS proxy data and validated using independent ASOS surface visibility measurements. Variability in the frequency of clear sky (aerosol) surface visibility retrievals larger than 20 dV is shown to be correlated with seasonal and interannual variability in fire detections, illustrating the importance of smoke from wildfires in regional haze events.
Cited articles
Alexandrov, M. D., Marshak, A., Cairns, B., Lacis, A. A., and Carlson, B. E.:
Automated cloud screening algorithm for MFRSR data, Geophys. Res. Lett.,
31, L04118, https://doi.org/10.1029/2003GL019105, 2004.
Anderson, G., Clough, S., Kneizys, F., Chetwynd, J., and Shettle, E.: AFGL
Atmospheric Constituent Profiles (0–120 km), Air Force Geophysics
Laboratory, AFGL-TR-86-0110, Environmental Research Papers, no. 954., 1986.
Ångström, A.: Parameters of atmospheric turbidity, Tellus XVI, 1,
64–75, 1964.
Cachorro, V. E., Duran, P., Vergaz, R., and de Frutos, A. M.: Measurements of the
atmospheric turbidity of the north-centre continental area in Spain:
spectral aerosol optical depth and Angstrom turbidity parameters, J.
Aerosol Sci., 31, 687–702, https://doi.org/10.1016/S0021-8502(99)00552-2, 2000.
Chen, Y. -C., Hamre, B., Frette, Q., Muyimbwa, D., Blindheim, S., Stebel, K.,
Sobolewski, P., Toledano, C., and Stamnes, J.: Aerosol optical properties in
Northern Norway and Svalbard, Appl. Opt., 55, 660–672.
https://doi.org/10.1364/AO.55.000660, 2016.
Chubarova, N., Nezval', Ye., Sviridenkov, I., Smirnov, A., and Slutsker, I.: Smoke aerosol and its radiative effects during extreme fire event over Central Russia in summer 2010, Atmos. Meas. Tech., 5, 557–568, https://doi.org/10.5194/amt-5-557-2012, 2012.
Chubarova, N. E., Nezval', E. I., Belikov, I. B., Gorbarenko, E. V., Eremina, I. D.,
Zhdanova, E. Yu., Korneva, I. A., Konstantinov, P. I., Lokoshchenko, M. A.,
Skorokhod, A. I., and Shilovtseva, O. A.: Climatic and Environmental Characteristics
of Moscow Megalopolis According to the Data of the Moscow State University
Meteorological Observatory over 60 Years, Russ. Meteorol. Hydro+., 39, 602–613, https://doi.org/10.3103/S1068373914090052, 2014.
Chubarova, N. Y., Poliukhov, A. A., and Gorlova, I. D.: Long-term variability of aerosol optical thickness in Eastern Europe over 2001–2014 according to the measurements at the Moscow MSU MO AERONET site with additional cloud and NO2 correction, Atmos. Meas. Tech., 9, 313–334, https://doi.org/10.5194/amt-9-313-2016, 2016.
Eck, T. F., Holben, B. N., Reid, J. S., Dubovik, O., Smirnov, A., O'Neill, N. T.,
Slutsker, I., and Kinne, S.: Wavelength dependence of the optical biomass
burning, urban, and desert dust aerosol, J. Geophys. Res., 104,
31333–31350, 1999.
Eck, T. F., Holben, B. N., Reid, J. S., Sinyuk, A., Hyer, E. J., O'Neill, N. T., Shaw,
G. E., Vande Castle, J. R., Chapin, F. S., Dubovik, O., Smirnov, A., Vermote, E.,
Schafer, J. S., Giles, D., Slutsker, I., Sorokine, M., and Newcomb, W. W.: Optical
properties of boreal region biomass burning aerosols in central Alaska and
seasonal variation of aerosol optical depth at an Arctic coastal site, J.
Geophys. Res., 114, D11201, https://doi.org/10.1029/2008JD010870, 2009.
Freund, J.: Aerosol optical depth in the Canadian Arctic, Atmos. Ocean,
21, 158–167, 1983.
Glantz, P., Bourassa, A., Herber, A., Iversen, T., Karlsson, J., Kirkevåg,
A., Maturilli, M., Seland, Ø., Stebel, K., Struthers, H., Matthias, M., and
Thomason, L.: Remote sensing of aerosols in the Arctic for an evaluation of
global climate model simulations, J. Geophys. Res.-Atmos., 119,
8169–8188, https://doi.org/10.1002/2013JD021279, 2014.
Gorbarenko, E. V. and Rublev, A. N.: Long-term changes in the aerosol optical
thickness in Moscow and correction under strong atmospheric turbidity,
Izv. Atmos. Ocean Phy+., 52, 188–195, 2016.
Herber, A., Thomason, L. W., Gernandt, H., Leiterer, U., Nagel, D., Schulz, K.,
Kaptu, J., Albrecht, T., and Notholt, J.: Continuous day and night aerosol optical
depth observations in the Arctic between 1991 and 1999, J. Geophys. Res., 107, 4097, https://doi.org/10.1029/2001JD000536, 2002.
Hoffmann, A., Ritter, C., Stock, M., Maturilli, M., Eckhardt, S., Herber, A., and
Neuber, R.: Lidar measurements of the Kasatochi aerosol plume in August and
September 2008 in Ny-Ålesund, Spitsbergen, J. Geophys. Res., 115, D00L12, https://doi.org/10.1029/2009JD013039, 2010.
Holben, B. N., Eck, T. F., Slutsker, I., Tanre, D., Buis, J. P., Setzer, A., Vermote,
E., Reagan, J. A., Kaufman, Y. J., Nakadjima, T., Lavenu, F., Jankowiak, I., and
Smirnov, A.: AERONET - A federated instrument network and data archive for
aerosol characterization, Rem. Sens. Environ., 66, 1–16, 1988.
Holben, B. N., Tanre, D., Smirnov, A., Eck, T. F., Slutsker, I., Abuhassan, N.,
Newcomb, W. W., Schafer, J. S., Chatenet, B., Lavenu, F., Kaufman, Y. J., Vande
Castle, J., Setzer, A., Markham, B., Clark, D., Frouin, R., Halthore, R., Karneli, A.,
O'Neill, N. T., Pietras, C., Pinker, R. T., Voss, K., and Zibordi, G.: An emerging
ground-based aerosol climatology: Aerosol optical depth from AERONET,
J. Geophys. Res., 106, 12067–12097, https://doi.org/10.1016/S0034-4257(98)00031-5, 2001.
IPCC: Climate Change 2013: The Physical Science Basis, Intergovernmental
Panel on Climate Change, 2013, 1552 pp. (electronic resource), available at:
http://www.climatechange2013.org/images/report/WG1AR5_ALL_FINAL.pdf (last access: 5 October 2020), 2013.
Isaksen, K., Nordli, O., Forland, E. J., Lupikasza, E., Eastwood, S., and
Niedzwiedz, T.: Recent warming on Spitsbergen – Influence of atmospheric
circulation and sea ice cover, J. Geophys. Res.-Atmos., 121, 11913–11931, https://doi.org/10.1002/2016JD025606, 2016.
Kabanov, D. M. and Sakerin, S. M.: About method of atmospheric aerosol optical
thickness determination in near-spectral range, Atmos. Ocean Opt., 10, 540–545, 1997.
Kabanov, D. M., Veretennikov, V. V., Voronina, Yu. V., Sakerin, S. M., and Turchinovich, Yu. S.: Information system for network sunphotometers, Atmos. Ocean Opt., 22, 121–127, https://doi.org/10.1134/S1024856009010187,
2009.
Kabanov, D. M. and Sakerin, S. M.: Comparison of assessment techniques of fine and
coarse component aerosol optical depth of the atmosphere from measurement in
the visible spectrum, in: Proc. SPIE., 22nd International Symposium Atmospheric and Ocean
Optics: Atmospheric Physics, Tomsk, Russia, 100353D, https://doi.org/10.1117/12.2248657. 2016.
Kabanov, D. M., Sakerin, S. M., Kruglinsky, I. A., Ritter, C., Sobolewski, P. S., and
Zielinski, T.: Comparison of atmospheric aerosol optical depths measured with
different sun photometers in three regions of Spitsbergen Archipelago, in: Proc. SPIE., 24th International Symposium on Atmospheric and Ocean Optics:
Atmospheric Physics, Tomsk, Russia, 13 December 2018, https://doi.org/10.1117/12.2503949,
2018.
Kabanov, D. M., Sakerin, S. M., and Ritter, C.: Preparing time series of observations
of atmospheric aerosol optical depth (AOD) at two stations on Spitsbergen
Archipelago and selecting methods of extracting the contributions of fine
and coarse AOD components, in: Proc. SPIE., 25th International Symposium
on Atmospheric and Ocean Optics: Atmospheric Physics, Novosibirsk, Russia, 18 December 2019, https://doi.org/10.1117/12.2539926, 2019a.
Kabanov, D. M., Sakerin, S. M., and Turchinovich, Yu, S.: Interannual and seasonal variations in the atmospheric aerosol optical depth in the region of Tomsk (1995–2018), Atmospheric and Ocean Optics, 32, 663–670, https://doi.org/10.1134/S1024856019060071, 2019b.
Kasten, F. and Young, A. T.: Revised optical air mass tables and approximation
formula, Appl. Opt., 28, 4375–4738, https://doi.org/10.1364/AO.28.004735, 1989.
Kondratyev, K. Ya., Ivlev, L. S., Krapivin, V. F., and Varotsos, C. A.: Atmospheric
aerosol properties, formation processes, and impacts: from nano- to global
scales, Springer/PRAXIS, Chichester, U.K., 572 pp., 2006.
Li, J., Carlson, B. E., Dubovik, O., and Lacis, A. A.: Recent trends in aerosol optical properties derived from AERONET measurements, Atmos. Chem. Phys., 14, 12271–12289, https://doi.org/10.5194/acp-14-12271-2014, 2014.
Markowicz, K. M., Pakszys, P., Ritter, C., Zielinski, T., Udisti, R., Cappelletti,
D., Mazzola, M., Shiobara, M., Xian, P., Zawadzka, O., Lisok, J., Petelski, T.,
Makuch, P., and Karasiński, G.: Impact of North American intense fires on
aerosol optical properties measured over the European Arctic in July 2015,
J. Geophys. Res. -Atmos, 121, 14487–14512, https://doi.org/10.1002/2016JD025310, 2016.
Mazzola, M., Stone, R. S., Herber, A., Tomasi, C., Lupi, A., Vitale, V., Lanconelli, C., Toledano, C., Cachorro, V. E., O’Neill, N. T., Shiobara, M., Aaltonen, V., Stebel, K., Zielinski, T., Petelski, T., Ortiz de Galisteo, J.-P., Torres, B., Berjon, A., Goloub, P., Li, Z., Blarel, L., Abboud, I., Cuevas, E., Stock, M., Schulz, K.-H., Virkkula, A.: Evaluation of sun photometer capabilities for retrievals
of aerosol optical depth at high latitudes: The POLAR-AOD intercomparison
campaigns, Atmos. Environ., 52, 4–17, https://doi.org/10.1016/j.atmosenv.2011.07.042, 2012.
Michalsky, J., Denn, F., Flynn, C., Hodges, G,, Kiedron, P., Koontz, A., Schlemmer,
J., and Schwartz, S. E.: Climatology of aerosol optical depth in north-central
Oklahoma: 1992–2008, J. Geophys. Res., 115, D07203, https://doi.org/10.1029/2009JD012197, 2010.
Lund Myhre, C., Toledano, C., Myhre, G., Stebel, K., Yttri, K. E., Aaltonen, V., Johnsrud, M., Frioud, M., Cachorro, V., de Frutos, A., Lihavainen, H., Campbell, J. R., Chaikovsky, A. P., Shiobara, M., Welton, E. J., and Tørseth, K.: Regional aerosol optical properties and radiative impact of the extreme smoke event in the European Arctic in spring 2006, Atmos. Chem. Phys., 7, 5899–5915, https://doi.org/10.5194/acp-7-5899-2007, 2007.
Ohvril, H., Teral, H., Neiman, L., Uustare, M., Tee, M., Russak, V., Kallis, A.,
Okulov, O., Terez, E., Terez, G., Guschin, G., Abakumova, G., Gorbarenko, E.,
Tsvetkov, A., and Laulainen, N.: Global dimming and brightening versus
atmospheric column transparency, Europe, 1906–2007, J. Geophys. Res., 114,
D00D12, https://doi.org/10.1029/2008JD010644, 2009.
O'Neill, N. T., Eck, T. F., Smirnov, A., Holben, B. N., and Thulasiraman, S.:
Spectral discrimination of coarse and fine mode optical depth, J. Geophys.
Res., 108, 4559–4573, https://doi.org/10.1029/2002JD002975, 2003.
Pakszys, Ð. and Zielinski, T.: Aerosol optical properties over Svalbard: a
comparison between Ny-Ålesund and Hornsund, Oceanologia, 2017,
431–444, https://doi.org/10.1016/j.oceano.2017.05.002, 2017.
Plakhina, I. N., Pankratova, N. V., and Makhotkina, E. L.: Variations in the
atmospheric aerosol optical depth from the data obtained at the Russian
actinometric network in 1976–2006, Izv. Atmos. Ocean Phy+., 45,
456–466, 2009.
Putaud, J. P., Cavalli, F., Martins dos Santos, S., and Dell'Acqua, A.: Long-term trends in aerosol optical characteristics in the Po Valley, Italy, Atmos. Chem. Phys., 14, 9129–9136, https://doi.org/10.5194/acp-14-9129-2014, 2014.
Quinn, P., Shaw, G., Andrews, E., Dutton, E. G., Ruoho-Airola, T., and Gong, S. L.: Arctic haze: current trends and knowledge gaps, Tellus, 59,
99–114, https://doi.org/10.1111/j.1600-0889.2006.00238.x, 2007.
Radionov, V. F. and Marshunova, M. S.: Long-term variations in the turbidity of
the Arctic atmosphere in Russia, Atmos. Ocean, 30, 531–549, 1992.
Sakerin, S. M. and Kabanov, D. M.: Spectral dependence of the atmospheric aerosol
optical depth in the wavelength range from 0.37 to 4 µm, Atmos. Ocean Opt., 20, 141–149, 2007a.
Sakerin, S. M. and Kabanov, D. M.: Correlations between the parameters of
Angström formula and aerosol optical thickness of the atmosphere in the
wavelength range from 1 to 4 µm, Atmos. Ocean Opt.,
20, 200–206, 2007b.
Sakerin, S. M., Gorbarenko, E. V., and Kabanov, D. M.: Peculiarities of many-year
variations of atmospheric aerosol optical thickness and estimates of
influence of different factors, Atmos. Ocean Opt., 21, 540–545, 2008a.
Sakerin, S. M., Kabanov, D. M., Smirnov, A. V., and Holben, B. N.: Aerosol optical depth
of the atmosphere over ocean in the wavelength range 0.37-4 µm,
Int. J. Remote Sens., 29, 2519–2547, https://doi.org/10.1080/01431160701767492, 2008b.
Sakerin, S. M., Kabanov, D. M., Nasrtdinov, I. M., Turchinovich, S. A., and
Turchinovich, Yu. S.: The results of two-point experiments on the estimation of the urban anthropogenic effect on the characteristics of atmospheric
transparency, Atmos. Ocean Opt., 23, 88–94,
https://doi.org/10.1134/S1024856010020028, 2010.
Sakerin, S. M., Kabanov, D. M., Rostov, A. P., Turchinovich, S. A., and Knyazev, V. V.:
Sun photometers for measuring spectral air transparency in stationary and
mobile conditions, Atmos. Ocean Opt., 26, 352–356, https://doi.org/10.1134/S102485601304012X, 2013.
Sakerin, S. M., Beresnev, S. A., Kabanov, D. M., Kornienko, G. I., Nikolashkin, S. V.,
Poddubny, V. A., Tashchilin, M. A., Turchinovich, Yu. S., Holben, B. N., and Smirnov,
A.: Analysis of approaches to modeling the annual and spectral behaviors of
atmospheric aerosol optical depth in Siberia and Primorye, Atmos. Ocean Opt., 28, 145–157, https://doi.org/10.1134/S1024856015020104,
2015.
Sakerin, S. M., Kabanov, D. M., Radionov, V. F., Chernov, D. G., Turchinovich, Yu. S.,
Lubo-Lesnichenk, K. E., and Prakhov, A. N.: Generalization of results of
atmospheric aerosol optical depth measurements on Spitsbergen Archipelago in
2011–2016, Atmos. Ocean Opt., 31, 163–170,
https://doi.org/10.1134/S1024856018020112, 2018a.
Sakerin, S. M., Golobokova, L. P., Kabanov, D. M., Pol'kin, V. V., and Radionov, V. F.:
Zonal distribution of aerosol physicochemical characteristics in the Eastern
Atlantic, Atmos. Ocean Opt., 31, 492–501, https://doi.org/10.1134/S1024856018050160, 2018b.
Schuster, G. L., Dubovik, O., and Holben, B. N.: Angstrom exponent and bimodal
aerosol size distributions, J. Geophys. Res., 111, D07207,
https://doi.org/10.1029/2005JD006328, 2006.
Shaw, G. E.: Atmospheric turbidity in the Polar regions, J. Appl. Meteorol., 21, 1080–1088, https://doi.org/10.1175/1520-0450(1982)021<1080:ATITPR>2.0.CO;2, 1982.
Shaw, G. E.: The Arctic haze phenomenon, Bull. Amer. Meteor. Soc., 76, 2403–2414, https://doi.org/10.1175/1520-0477(1995)076<2403:TAHP> 2.0.CO;2, 1995.
Shifrin, K. S.: Simple relationships for the Angstrom parameter of disperse
systems, Appl. Opt., 34, 4480–4485, 1995.
Sitnov, S. A., Gorchakov, G. I., Sviridenkov, M. A., Gorchakova, I. A., Karpov, A. V.,
and Kolesnikova, A. B.: Aerospace monitoring of smoke aerosol over the European
part of Russia in the period of massive forest and peatbog fires in
July–August of 2010, Atmos. Ocean Opt., 26,
265–280, https://doi.org/10.1134/S1024856013040143, 2013.
Stohl, A., Andrews, E., Burkhart, J. F., Forster, C., Herber, A., Hoch, S. W., Kowal,
D., Lunder, C., Mefford, T., Ogren, J. A., Sharma, S., Spichtinger, N., Stebel, K.,
Stone, R., Ström, J., Tørseth, K., Wehrli, C., and Yttri,
K. E.: Pan-Arctic enhancements of light absorbing aerosol concentrations due
to North American boreal forest fires during summer 2004, J. Geophys. Res., 111, D22214, https://doi.org/10.1029/2006JD007216, 2006.
Stohl, A., Berg, T., Burkhart, J. F., Fjǽraa, A. M., Forster, C., Herber, A., Hov, Ø., Lunder, C., McMillan, W. W., Oltmans, S., Shiobara, M., Simpson, D., Solberg, S., Stebel, K., Ström, J., Tørseth, K., Treffeisen, R., Virkkunen, K., and Yttri, K. E.: Arctic smoke – record high air pollution levels in the European Arctic due to agricultural fires in Eastern Europe in spring 2006, Atmos. Chem. Phys., 7, 511–534, https://doi.org/10.5194/acp-7-511-2007, 2007.
Stone, R. S., Anderson, G. P., Shettle, E. P., Andrews, E., Loukachine, K., Dutton,
E. G., Schaaf, C., and Roman III, M. O.: Radiative impact of boreal smoke in the
Arctic: Observed and modelled, J. Geophys. Res., 113, D14S16, https://doi.org/10.1029/2007JD009657, 2008.
Sviridenkov, M. A.: Retrieval of atmospheric aerosol characteristics from
spectral measurements of transparency and small-angle scattering, Atmos.
Ocean Opt., 14, 1022–1025, 2001.
Toledano, C., Cachorro, V., Gausa, M., Stebel, K., Aaltonen, V., Berjon, A., Ortis,
J. P., de Frutos, A. M., Bennouna, Y., Blindheim, S., Myhre, C. L., Zibordi, G.,
Wehrli, C., Kratzer, S., Hakanson, B., Carlund, T., de Leuww, G., and Herber, A.:
Overview of sun photometer measurements of aerosol properties in Scandinavia
and Svalbard, Atmos. Environ., 52, 18–28,
https://doi.org/10.1016/j.atmosenv.2011.10.022, 2012.
Tomasi, C., Lupi, A., Mazzola, M., Stone, R. S., Dutton, E. G., Herber, A., Radionov, V. F., Holben, B., Sorokin, M., Sakerin, S. M., Terpugova, S. A., Lanconelli, C.,
Petkov, B., and Vitale, V.: An update of the long-term trend of aerosol optical
depth in the polar regions using POLAR-AOD measurements performed during in
International Polar Year, Atmos. Environ., 52, 29–47,
https://doi.org/10.1016/j.atmosenv.2012.02.055, 2012.
Tomasi, C., Kokhanovsky, A. A., Lupi, A., Ritter, C., Smirnov, A., Mazzola, M.,
Stone, R. S., Lanconelli, C., Vitale, V., Holben, B. N., Nyeki, S., Wehrli, C.,
Altonen, V., de Leeuw, G., Rodriguez, E., Herber, A. B., Stebel, K., Stohl, A.,
O'Neill, N. T., Radionov, V. F., Zielinski, T., Petelski, T., Sakerin, S. M.,
Kabanov, D. M., Xue, Y., Mei, L., Istomina, L., Wagener, R., McArthur, B.,
Sobolewski, P. S., Butler, J., Kivi, R., Courcoux, Y., Larouche, P., Broccardo, S., and
Piketh, S. J.: Aerosol remote sensing in polar regions, Earth-Sci. Rev.,
140, 108–157, https://doi.org/10.1016/j.earscirev.2014.11.001, 2015.
Tørseth, K., Aas, W., Breivik, K., Fjæraa, A. M., Fiebig, M., Hjellbrekke, A. G., Lund Myhre, C., Solberg, S., and Yttri, K. E.: Introduction to the European Monitoring and Evaluation Programme (EMEP) and observed atmospheric composition change during 1972–2009, Atmos. Chem. Phys., 12, 5447–5481, https://doi.org/10.5194/acp-12-5447-2012, 2012.
Twitty, J. T.: The inversion of aureole measurements to derive aerosol size
distributions, J. Atmos. Sci., 32, 584–591, https://doi.org/10.1175/1520-0469(1975)032<0584:TIOAMT>2.0.CO;2, 1975.
Vinogradova, A. A., Smirnov, N. S., Korotkov, V. N., and Romanovskay, A. A.: Forest
fires in Siberia and the far east: emissions and atmospheric transport of
black carbon to the Arctic, Atmos. Ocean Opt., 28, 566–574. https://doi.org/10.1134/S1024856015060184, 2015.
Walczowski, W. and Piechura, J.: Influence of the West Spitsbergen Current on
the local climate. Int. J. Climatol, 31, 1088–1093, https://doi.org/10.1002/joc.2338,
2011.
Weller, M., Schulz, E., Leiterer, U., Naebert, T., Herber, A., and Thomason, L. W.:
Ten years of aerosol optical depth observation at the Lindenberg
meteorological observatory, Contr. Atmos. Phys. 71, 387–400,
1998.
WMO: WMO/GAW Expert Workshop on a global surface-based network for long term
observations of column aerosol optical properties, editied by: Baltensperger U.,
Barrie, L., and Wehrli, C., Report GAW 162 – WMO/GAW, Davos, March 2005 (WMO TD No.
1287), 144 pp., available at: https://library.wmo.int/doc_num.php?explnum_id=9299 (last access: 5 October 2020), 2005.
WMO: WMO/GAW report no. 183, operations handbook – ozone observations with a
Dobson spectrophotometer, available at: https://www.wmo.int/pages/prog/arep/gaw/documents/GAW183-Dobson-WEB.pdf (last access: 5 October 2020), 85 pp., 2008.
Xia, X. G.: Variability of aerosol optical depth and Ångström
wavelength exponent derived from AERONET observations in recent decades,
Environ. Res. Lett., 6, 044011, https://doi.org/10.1088/1748-9326/6/4/044011, 2011.
Zhdanova, E. Yu., Khlestova, Yu. O., and Chubarova, N. Y.: Trends in Atmospheric Aerosol Characteristics in Moscow derived from Multiyear AERONET Measurements, Atmos. Ocean Opt., 32, 534–539, https://doi.org/10.1134/S1024856019050191, 2019.
Zhuravleva, T. B., Kabanov, D. M., Nasrtdinov, I. M., Russkova, T. V., Sakerin, S. M., Smirnov, A., and Holben, B. N.: Radiative characteristics of aerosol during extreme fire event over Siberia in summer 2012, Atmos. Meas. Tech., 10, 179–198, https://doi.org/10.5194/amt-10-179-2017, 2017.
Search articles
Download
Short summary
Long-term photometer measurements of two sites on Spitsbergen, Barentsburg and Ny-Ålesund, in the European Arctic are presented and compared. We find slightly higher aerosol optical depths at Barentsburg and attribute this to a higher concentration of small particles.
Long-term photometer measurements of two sites on Spitsbergen, Barentsburg and Ny-Ålesund, in...
Atmospheric Measurement Techniques
An interactive open-access journal of the European Geosciences Union
All site content, except where otherwise noted, is licensed under the Creative Commons Attribution 4.0 License.