Articles | Volume 15, issue 16
https://doi.org/10.5194/amt-15-4767-2022
https://doi.org/10.5194/amt-15-4767-2022
Research article
 | 
23 Aug 2022
Research article |  | 23 Aug 2022

Intercomparison of upper tropospheric and lower stratospheric water vapor measurements over the Asian Summer Monsoon during the StratoClim campaign

Clare E. Singer, Benjamin W. Clouser, Sergey M. Khaykin, Martina Krämer, Francesco Cairo, Thomas Peter, Alexey Lykov, Christian Rolf, Nicole Spelten, Armin Afchine, Simone Brunamonti, and Elisabeth J. Moyer

Data sets

Mission: StratoClim DLR (German Aerospace Center) https://halo-db.pa.op.dlr.de/mission/101

The Cirrus Guide II In-situ Aircraft Data Set M. Krämer, C. Rolf, and N. Spelten https://doi.org/10.34730/266ca2a41f4946ff97d874bfa458254c

MLS/Aura Level 2 Water Vapor (H2O) Mixing Ratio V004, Greenbelt A. Lambert, W. Read, and N. Livesey https://doi.org/10.5067/Aura/MLS/DATA2009

MLS/Aura Level 2 Water Vapor (H$_2$O) Mixing Ratio V005 A. Lambert, W. Read, and N. Livesey https://doi.org/10.5067/Aura/MLS/DATA2508

Model code and software

Scripts for Singer et al. (2022): "Intercomparison of upper tropospheric and lower stratospheric water vapor measurements over the Asian Summer Monsoon during the StratoClim campaign" (v1.0) C. E. Singer https://doi.org/10.5281/zenodo.6954851

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Short summary
In situ measurements of water vapor in the upper troposphere are necessary to study cloud formation and hydration of the stratosphere but challenging due to cold–dry conditions. We compare measurements from three water vapor instruments from the StratoClim campaign in 2017. In clear sky (clouds), point-by-point differences were <1.5±8 % (<1±8 %). This excellent agreement allows detection of fine-scale structures required to understand the impact of convection on stratospheric water vapor.