Articles | Volume 15, issue 11
https://doi.org/10.5194/amt-15-3555-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/amt-15-3555-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Determination of atmospheric column condensate using active and passive remote sensing technology
Huige Di
School of Mechanical and Precision Instrument Engineering, Xi'an
University of Technology, Xi'an 710048, China
Yun Yuan
School of Mechanical and Precision Instrument Engineering, Xi'an
University of Technology, Xi'an 710048, China
Qing Yan
School of Mechanical and Precision Instrument Engineering, Xi'an
University of Technology, Xi'an 710048, China
Wenhui Xin
School of Mechanical and Precision Instrument Engineering, Xi'an
University of Technology, Xi'an 710048, China
Shichun Li
School of Mechanical and Precision Instrument Engineering, Xi'an
University of Technology, Xi'an 710048, China
Jun Wang
School of Mechanical and Precision Instrument Engineering, Xi'an
University of Technology, Xi'an 710048, China
Yufeng Wang
School of Mechanical and Precision Instrument Engineering, Xi'an
University of Technology, Xi'an 710048, China
Lei Zhang
College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, China
Dengxin Hua
CORRESPONDING AUTHOR
School of Mechanical and Precision Instrument Engineering, Xi'an
University of Technology, Xi'an 710048, China
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Short summary
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We put forward a new algorithm for joint observation of the cloud boundary by lidar and Ka-band millimetre-wave cloud radar. Cloud cover and boundary distribution characteristics are analysed from December 2020 to November 2021 in Xi'an. More than 34 % of clouds appear as a single layer every month. The maximum and minimum normalized cloud cover occurs in summer and winter, respectively. The study can provide more information on aerosol–cloud interactions and forecasting numerical models.
Guanglie Hong, Yu Dong, and Huige Di
Atmos. Meas. Tech. Discuss., https://doi.org/10.5194/amt-2022-69, https://doi.org/10.5194/amt-2022-69, 2022
Revised manuscript not accepted
Short summary
Short summary
According to the absorption spectrum characteristics of oxygen A-band, a comprehensive budget is made in connection with various errors. The main purpose is to select a group of detection wavelengths with excellent performance and small error to match the evaluated radar system model, so as to provide a reference idea for the actual establishment of the experimental system in the future.
Cited articles
Babb D. M., Verlinde J., and Rust B. W.: The Removal of Turbulent Broadening in Radar Doppler Spectra Using Linear Inversion with Double-Sided Constraints, J. Atmos. Ocean. Tech, 17, 1583–1595, https://doi.org/10.1175/1520-0426(2000)017<1583:TROTBI>2.0.CO;2, 1999.
Behrendt, A. and Nakamura, T.: Calculation of the calibration constant of polarization lidar and its dependency on atmospheric temperature, Opt. Express, 10, 805–17, https://doi.org/10.1364/OE.10.000805, 2002.
Cooney, J.: Measurement of atmospheric temperature profiles by raman backscatter, J. Appl. Meteorol. Clim., 11, 108–112, https://doi.org/10.1175/1520-0450(1972)011<0108:moatpb>2.0.co;2, 1972.
Frehlich, R., Hannon, S. M., and Henderson, S. W.: Performance of a 2-m
coherent doppler lidar for wind measurements, J. Atmos. Ocean. Tech., 11, 1517–1528, https://doi.org/10.1175/1520-0426(1994)011<1517:POACDL>2.0.CO;2, 1994.
Gossard, E. E.: Measurement of cloud droplet size spectra by doppler radar,
J. Atmos. Ocean. Tech., 11, 712–726, https://doi.org/10.1175/1520-0426(1994)011<0712:MOCDSS>2.0.CO;2, 1994.
Gossard, E. E., Snider, J. B., Clothiaux, E. E., Martner, B., and Frisch,
A. S.: The potential of 8-mm radars for remotely sensing cloud drop size
distributions, J. Atmos. Ocean. Tech., 14, 76–87, https://doi.org/10.1175/1520-0426(1997)014<0076:TPOMRF>2.0.CO;2, 1996.
Gu, X. and Zhang B.: Vapor sink and latent heat of condensation in the
atmosphere and the parameterization of cumulus convection, Acta Meteorol.
Sin., 64, 790–795, https://doi.org/10.1016/S1872-2032(06)60022-X, 2006.
Iwasaki, S., Seguchi, T., Okamoto, H., Sato, K., Katagiri, S., Fujiwara, M., Shibata, T., Tsuboki, K., Ono, T., and Sugidachi, T.:
Large-and-sparse-particle clouds (lsc): clouds that are subvisible for
space-borne lidar and observable for space-borne cloud radar, Polar Sci.,
21, 117–123, https://doi.org/10.1016/j.polar.2019.05.003, 2019.
Jalihal, C., Srinivasan, J., and Chakraborty, A.: Modulation of indian
monsoon by water vapor and cloud feedback over the past 22,000 years, Nat.
Commun., 10, 5701, https://doi.org/10.1038/s41467-019-13754-6, 2019.
Kollias, P., Albrecht, B. A., Lhermitte, R., and Savtchenko, A.: Radar
observations of updrafts, downdrafts, and turbulence in fair-weather cumuli,
J. Atmos. Sci., 58, 1750–1766, https://doi.org/10.1175/1520-0469(2001)058<1750:ROOUDA>2.0.CO;2, 2001.
Kollias, P., Albrecht, B. A., and Marks, F.: Why mie? accurate observations
of vertical air velocities and raindrops using a cloud radar,
B. Am. Meteorol. Soc., 83, 1471–1483, https://doi.org/10.1175/BAMS-83-10-1471, 2002.
Kollias, P., Rémillard, J., Luke, E., and Szyrmer, W.: Cloud radar
doppler spectra in drizzling stratiform clouds: 1. forward modeling and
remote sensing applications, J. Geophys. Res.-Atmos., 116, D13201, https://doi.org/10.1029/2010JD015237, 2011.
Lei, H., Jin, D., Wei, C., and Shen, Z.: An airborne microwave
radiometer and measurements of cloud liquid water, Chinese Sci Bull.,
48, 82–87, https://doi.org/10.1360/03wd0462, 2003.
Leinonen, J., Lebsock, M. D., Stephens, G. L., and Suzuki K.: Improved retrieval of cloud liquid water from CloudSat and MODIS, J. Appl. Meteorol. Clim., 55, 1831–1844, https://doi.org/10.1175/JAMC-D-16-0077.1, 2016.
Liu, F. and Yi, F.: Spectrally resolved raman lidar measurements of
gaseous and liquid water in the atmosphere, Appl. Optics, 52, 6884–6895,
https://doi.org/10.1364/AO.52.006884, 2013.
Lottman, B. T. and Frehlich, R. G.: Evaluation of vertical winds near and
inside a cloud deck using coherent doppler lidar, J. Atmos. Ocean. Tech.,
18, 1377–1386, https://doi.org/10.1175/1520-0426(2001)018<1377:EOVWNA>2.0.CO;2, 2001.
Luke, E. P. and Kollias, P.: Separating Cloud and Drizzle Radar Moments during Precipitation Onset Using Doppler Spectra, J. Atmos. Ocean. Tech., 30, 1656–1671, https://doi.org/10.1175/JTECH-D-11-00195.1, 2013.
Mao, F., Gong, W., Li, J., and Zhang, J.: Cloud detection and parameter
retrieval based on improved differential zero-crossing method for mie lidar,
Acta Optica Sinica, 30, 3097–3102, https://doi.org/10.3788/AOS20103011.3097, 2010.
O'Connor, E. J., Hogan, R. J., and Illingworth, A. J.: Retrieving
stratocumulus drizzle parameters using doppler radar and lidar, J. Appl.
Meteorol. Clim., 44, 14–27, https://doi.org/10.1175/JAM-2181.1, 2005.
Shupe, M. D., Kollias, P., Persson, P. O. G., and Mcfarquhar, G. M.: Vertical Motions in Arctic Mixed-Phase Stratiform Clouds, J. Atmos. Sci., 65, 1304-1322, https://doi.org/10.1175/2007JAS2479.1, 2007.
Shupe, M. D., Kollias, P., Poellot, M., and Eloranta, E.: On deriving
vertical air motions from cloud radar doppler spectra, J. Atmos. Ocean. Tech., 25, 547–557, https://doi.org/10.1175/2007JTECHA1007.1, 2008.
Su, J., Mccormick, M. P., Wu, Y., Lee, R. B., Lei, L., and Liu, Z.: Cloud
temperature measurement using rotational raman lidar, J. Quant. Spectrosc. Ra., 125, 45–50, https://doi.org/10.1016/j.jqsrt.2013.04.007, 2013.
Su, T. and Feng, G. L.: The characteristics of the summer atmospheric water
cycle over China and comparison of ERA-Interim and MERRA reanalysis, Acta
Phys. Sin., 63, 493–505, https://doi.org/10.7498/aps.63.249201, 2014.
Williams, C. R., Beauchamp, R. M., and Chandrasekar, V.: Vertical air
motions and raindrop size distributions estimated using mean doppler
velocity difference from 3- and 35-ghz vertically pointing radars, IEEE T.
Geosci. Remote., 54, 1–13, https://doi.org/10.1109/TGRS.2016.2580526, 2016.
Wu, D., Wang, Z., Wechsler, P., Mahon, N., and Heesen, B.: Airborne compact
rotational raman lidar for temperature measurement, Opt. Express, 24,
A1210–A1223, https://doi.org/10.1364/OE.24.0A1210, 2016.
Yao, J. Q., Chen, Y. N., Zhao, Y., Guan, X. F., Mao, W. Y., and Yang, L. M.: Climatic and associated atmospheric water cycle changes over the Xinjiang, China, J. Hydrol., 585, 124823, https://doi.org/10.1016/j.jhydrol.2020.124823, 2020.
Yoshiaki, S., Yamanaka, M. D., Hiroyuki, H., Akira, W., Hiroshi, U., and
Yasuyuki, M.: Hierarchical structures of vertical velocity variations and
precipitating clouds near the baiu frontal cyclone center observed by the mu
and meteorological radars, J. Meteorol. Soc. Jpn., 75, 569–596,
https://doi.org/10.2151/jmsj1965.75.2_569, 2009.
Zhao, C., Wang, Y., Wang, Q., Li, Z., Wang, Z., and Liu, D.: A new cloud
and aerosol layer detection method based on micropulse lidar measurements, J.
Geophys. Res.-Atmos., 119, 6788–6802, https://doi.org/10.1002/2014JD021760, 2014.
Zheng, J., Liu, L., Zhu, K., Wu, J., and Wang, B.: A method for retrieving vertical air velocities in convective clouds over the tibetan plateau from tipex-iii cloud radar doppler spectra, Remote. Sens., 9, 964, https://doi.org/10.3390/rs9090964, 2017.
Zhou, L., Liu, Q., Liu, D., Xie, L., Qi, L., and Liu, X.: Validation of
modis liquid water path for oceanic nonraining warm clouds: implications on
the vertical profile of cloud water content, J. Geophys. Res.-Atmos., 121,
4855–4876, https://doi.org/10.1002/2015JD024499, 2016.
Zhou, Y., Cai, M., Tan, C., Mao, J., and Zhijin, H. U.: Quantifying the
cloud water resource: basic concepts and characteristics, J. Meteorol. Res.-Prc., 34, 1242–1255, https://doi.org/10.1007/s13351-020-9125-7, 2020.
Executive editor
The remote sensing observation of condensation water in cloud is realized by using active and passive remote sensing instruments. This is the first application, to our knowledge, of observations for atmospheric column condensate evaluation, which is significant for research on the hydrologic cycle and the assessment of cloud water resources.
The remote sensing observation of condensation water in cloud is realized by using active and...
Short summary
It is necessary to correctly evaluate the amount of cloud water resources in an area. Currently, there is a lack of effective observation methods for atmospheric column condensate evaluation. We propose a method for atmospheric column condensate by combining millimetre cloud radar, lidar and microwave radiometers. The method can realise determination of atmospheric column condensate. The variation of cloud before precipitation is considered, and the atmospheric column is deduced and obtained.
It is necessary to correctly evaluate the amount of cloud water resources in an area. Currently,...