Validation of AIRS/AMSU-A water vapor and temperature data with in situ aircraft observations from the surface to UT/LS from 87°N-67°S
Validation of AIRS/AMSU-A water vapor and temperature data with in situ aircraft observations from the surface to UT/LS from 87°N-67°S
Validation of the Atmospheric Infrared Sounder (AIRS)/Advanced Microwave Sounding Unit (AMSU-A) data set with in situ observations provides useful information on its application to climate and weather studies. However, different space/time averaging windows have been used in past studies, and questions remain on the variation of errors in space, such as between land/ocean and the Northern/Southern Hemispheres. In this study, in situ aircraft measurements of water vapor and temperature are compared with the AIRS/AMSU-A retrievals (Version 5 Level 2) from 87°N to 67°S and from the surface to the upper troposphere and lower stratosphere (UT/LS). By using a smaller comparison window (1 h and 22.5 km) than previous studies, we show that the absolute percentage difference of water vapor (|dH2Operc|) is ~20-60% and the absolute temperature difference (|dTemp|) is ~1.0-2.5 K. The land retrievals show improvements versus Version 4 by ~5% in water vapor concentration and ~0.2 K in temperature at 200-800 mbar. The land (ocean) retrievals are colder and drier (warmer and moister) than the in situ observations in the boundary layer, warmer and drier (warmer and moister) at the UT/LS. No significant differences between hemispheres are noted. Overall, future comparisons are suggested to be done within 4 h and 100 km in order to keep the errors from window sizes within ~10%. To constrain the uncertainties in previous validation results, we show that every 22.5 km (or 1 h) increment in window sizes contributes to ~2% |dH2Operc| and ~0.1 K |dTemp| increases. Key Points Improved validation of AIRS/AMSU-A water vapor and temperature Sensitivity of validation of space/time windows studied New validations over land, ocean, and Southern Hemisphere
AIRS, AMSU, relative humidity, validation, water vapor
6816-6836
Diao, Minghui
7ad51b7d-da5c-410c-8629-fa977560bf7e
Jumbam, Loayeh
737b94ab-4473-41a6-ad7a-791d85c9ab5e
Sheffield, Justin
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Wood, Eric F.
8352c1b4-4fd3-42fe-bd23-46619024f1cf
Zondlo, Mark A.
e68533b8-89bf-46b6-96fb-e4cfe5654769
27 June 2013
Diao, Minghui
7ad51b7d-da5c-410c-8629-fa977560bf7e
Jumbam, Loayeh
737b94ab-4473-41a6-ad7a-791d85c9ab5e
Sheffield, Justin
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Wood, Eric F.
8352c1b4-4fd3-42fe-bd23-46619024f1cf
Zondlo, Mark A.
e68533b8-89bf-46b6-96fb-e4cfe5654769
Diao, Minghui, Jumbam, Loayeh, Sheffield, Justin, Wood, Eric F. and Zondlo, Mark A.
(2013)
Validation of AIRS/AMSU-A water vapor and temperature data with in situ aircraft observations from the surface to UT/LS from 87°N-67°S.
Journal of Geophysical Research Atmospheres, 118 (12), .
(doi:10.1002/jgrd.50483).
Abstract
Validation of the Atmospheric Infrared Sounder (AIRS)/Advanced Microwave Sounding Unit (AMSU-A) data set with in situ observations provides useful information on its application to climate and weather studies. However, different space/time averaging windows have been used in past studies, and questions remain on the variation of errors in space, such as between land/ocean and the Northern/Southern Hemispheres. In this study, in situ aircraft measurements of water vapor and temperature are compared with the AIRS/AMSU-A retrievals (Version 5 Level 2) from 87°N to 67°S and from the surface to the upper troposphere and lower stratosphere (UT/LS). By using a smaller comparison window (1 h and 22.5 km) than previous studies, we show that the absolute percentage difference of water vapor (|dH2Operc|) is ~20-60% and the absolute temperature difference (|dTemp|) is ~1.0-2.5 K. The land retrievals show improvements versus Version 4 by ~5% in water vapor concentration and ~0.2 K in temperature at 200-800 mbar. The land (ocean) retrievals are colder and drier (warmer and moister) than the in situ observations in the boundary layer, warmer and drier (warmer and moister) at the UT/LS. No significant differences between hemispheres are noted. Overall, future comparisons are suggested to be done within 4 h and 100 km in order to keep the errors from window sizes within ~10%. To constrain the uncertainties in previous validation results, we show that every 22.5 km (or 1 h) increment in window sizes contributes to ~2% |dH2Operc| and ~0.1 K |dTemp| increases. Key Points Improved validation of AIRS/AMSU-A water vapor and temperature Sensitivity of validation of space/time windows studied New validations over land, ocean, and Southern Hemisphere
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Published date: 27 June 2013
Keywords:
AIRS, AMSU, relative humidity, validation, water vapor
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Local EPrints ID: 480772
URI: http://eprints.soton.ac.uk/id/eprint/480772
ISSN: 2169-8996
PURE UUID: bd6eef8d-b47f-47c7-af8c-9a60d9088bf0
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Date deposited: 09 Aug 2023 17:11
Last modified: 17 Mar 2024 03:40
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Contributors
Author:
Minghui Diao
Author:
Loayeh Jumbam
Author:
Eric F. Wood
Author:
Mark A. Zondlo
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