2019
DOI: 10.5194/hess-2019-387
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A daily/25 km short-latency rainfall product for data scarce regions based on the integration of the GPM IMERG Early Run with multiple satellite soil moisture products

Abstract: Rain gauges are unevenly spaced around the world with extremely low gauge density over developing countries. For instance, in some regions in Africa the gauge density is often less than one station per 10000 km 2 . The availability of rainfall data provided by gauges is also not always guaranteed in near real time or with a timeliness suited for agricultural and water resource management applications as gauges are also subject to malfunctions and regulations imposed by national authorities.A potential alternat… Show more

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Cited by 5 publications
(14 citation statements)
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“…In this study, we used the IMERG-Early and IMERG-Final products. The two products were upscaled to 0.25 • by using a box-shaped kernel with antialiasing, which was found to outperform simple spatial averaging, and half-hourly rainfall were accumulated to obtain a daily product [36].…”
Section: Data Setmentioning
confidence: 99%
“…In this study, we used the IMERG-Early and IMERG-Final products. The two products were upscaled to 0.25 • by using a box-shaped kernel with antialiasing, which was found to outperform simple spatial averaging, and half-hourly rainfall were accumulated to obtain a daily product [36].…”
Section: Data Setmentioning
confidence: 99%
“…In addition to rain gauges, and ground meteorological radars, meteorological and numerical weather prediction models and satellite observations can be used. However, both data sources rely directly or indirectly on ground observations (e.g., through assimilation for modelling or used as reference for satellite products), and hence their reliability over scarcely gauged areas is highly uncertain 9 .…”
Section: Introductionmentioning
confidence: 99%
“…The bottom up approach clearly distinguishes from the state-of-the-art top down method (i.e., GPM) as the rainfall signal is obtained\enhanced from the knowledge of the soil moisture signal, i.e., from the bottom up. This relatively new approach has been tested with different satellite sensors (e.g., Soil Moisture Ocean Salinity, SMOS, mission 15 , 16 ; Soil Moisture Active and Passive, SMAP, mission 17 ; and Advanced SCATterometer, ASCAT, sensor 18 ), and recently also by integrating multiple satellite soil moisture products 9 , 19 .…”
Section: Introductionmentioning
confidence: 99%
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