2023
DOI: 10.1039/d2ea00139j
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Long-term changes in precipitable water vapour over India derived from satellite and reanalysis data for the past four decades (1980–2020)

Abstract: India has tropical monsoon climate with significant regional variability in rainfall and temperature, where precipitation is closely connected to precipitable water vapour (PWV). Here, the satellite and reanalysis data are...

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Cited by 5 publications
(3 citation statements)
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“…One of our future considerations will be the most comprehensive comparison of GPS moisture content data with the well-established ERA5 reanalysis data from ECMWF. The work [11] confirms that ERA5 PW complies with GPS measurements, with correlation coefficient range from 0.93 to 0.99, the BIAS between ERA5 PW and GPS PW ranged from 0.24 to 0.49 cm. This indicates that GPS observations can accurately capture the observed PW variability.…”
Section: Comparison Of Long-term Pw Trends Based On Rs Meteorology An...supporting
confidence: 81%
“…One of our future considerations will be the most comprehensive comparison of GPS moisture content data with the well-established ERA5 reanalysis data from ECMWF. The work [11] confirms that ERA5 PW complies with GPS measurements, with correlation coefficient range from 0.93 to 0.99, the BIAS between ERA5 PW and GPS PW ranged from 0.24 to 0.49 cm. This indicates that GPS observations can accurately capture the observed PW variability.…”
Section: Comparison Of Long-term Pw Trends Based On Rs Meteorology An...supporting
confidence: 81%
“…Taking into account the surface temperature and pressure, the PWV values can be estimated from these delays with a low uncertainty. Nowadays this method is widely used for this purpose, including evaluation of results obtained from the global atmospheric models mentioned above (e.g., [46][47][48][49][50][51][52][53][54][55][56][57]).…”
Section: Evaluation Of the Precipitable Water Vapor (Pwv) From The Gl...mentioning
confidence: 99%
“…Most water vapor is present in the lower troposphere and plays a critical role during the precipitation process in the lower atmosphere as well as water circulation and climatic phenomena. Moreover, changes in the PW amount are also strongly associated with the global radiation balance, and they may affect the structure of atmospheric temperature and the characteristics of droughts and rainfall [4]. Furthermore, water vapor in the atmosphere provides the only major positive feedback for global warming [5][6][7], and it is predicted, based on both climate models and observations, that the amount of water vapor may tend to increase in response to the rise in the surface temperature [7][8][9].…”
Section: Introductionmentioning
confidence: 99%