Assessing the consistency of satellite-derived upper tropospheric humidity measurements
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Published:2022-12-02
Issue:23
Volume:15
Page:6949-6963
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ISSN:1867-8548
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Container-title:Atmospheric Measurement Techniques
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language:en
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Short-container-title:Atmos. Meas. Tech.
Author:
Shi Lei, Schreck III Carl J., John Viju O., Chung Eui-Seok, Lang TheresaORCID, Buehler Stefan A.ORCID, Soden Brian J.
Abstract
Abstract. Four upper tropospheric humidity (UTH) datasets derived
from satellite sounders are evaluated to assess their consistency as part of the activities for the Global Energy and Water Exchanges (GEWEX) water vapor assessment project. The datasets include UTH computed from brightness
temperature measurements of the 183.31±1 GHz channel of the Special
Sensor Microwave – Humidity (SSM/T-2), Advanced Microwave Sounding Unit-B
(AMSU-B), and Microwave Humidity Sounder (MHS) and from channel 12 of the
High-resolution Infrared Radiation Sounder (HIRS). The four datasets are
generally consistent in the interannual temporal and spatial variability of
the tropics. Large positive anomalies peaked over the central equatorial
Pacific region during El Niño events in the same phase with the increase of sea surface temperature (SST). Conversely, large negative anomalies were obtained during El Niño events when the tropical-domain average is
taken. The weakened ascending branch of the Pacific Walker circulation in
the western Pacific and the enhanced descending branches of the local Hadley circulation along the Pacific subtropics largely contributed to widespread drying areas and thus negative anomalies in the upper troposphere during El Niño events as shown in all four datasets. During a major El Niño event, UTH had higher correlations with the coincident precipitation (0.60 to 0.75) and with 200 hPa velocity potential (−0.42 to −0.64) than with SST (0.37 to 0.49). Due to differences in retrieval definitions and gridding procedures, there can be a difference of 3 %–5 % UTH between datasets on average, and larger magnitudes of anomaly values are usually observed in spatial maps of microwave UTH data. Nevertheless, the tropical-domain averaged anomalies of the datasets are close to each other with their differences being mostly less than 0.5 %, and more importantly the phases of the time series are generally consistent for variability studies.
Funder
National Oceanic and Atmospheric Administration
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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