From SMOS Soil Moisture to 3-hour Precipitation Estimates at 0.1° Resolution in Africa

نویسندگان

چکیده

Several recent studies have shown that knowledge of the spatiotemporal dynamics soil moisture intrinsically contains information on precipitation. In this study, we show how SMOS measurements can be used to generate a near-real-time precipitation product with spatial resolution 0.1° and temporal 3 h. The principle consists assimilating data into model simulates evolution moisture, which is forced by satellite product. assimilation leads an adjustment rates. Using from more than 200 rain gauges set up in Africa between 2010 2021, PrISM algorithm (for Precipitation Inferred Soil Moisture) almost systematically improves initial One original features study IMERG-Early product, has finer (0.1°) (~0.25°). Despite this, methodology reduces both RMSE bias IMERG-Early. reduced 8.0 6.3 mm/day, absolute 0.81 0.63 mm/day average over gauges. performs even slightly better IMERG-Final terms (6.8 for IMERG-Final) but scores are obtained (0.35 mm/day), utilizes network field correct biases 2.5-month delay. Therefore, use advantageous alternative gauge debiasing rainfall products real time.

برای دانلود رایگان متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Comparing soil moisture retrievals from SMOS and ASCAT over France

The first products derived over France in 2010 from the L-band brightness temperatures (Tb) measured by the SMOS (Soil Moisture and Ocean Salinity) satellite, launched in November 2009, were compared with the surface soil moisture (SSM) estimates produced by the C-band Advanced Scatterometer, ASCAT, launched in 2006 on board METOP-A. SMOS and ASCAT SSM products were compared with the simulation...

متن کامل

1 SMOS - IC : An alternative SMOS soil moisture and 2 vegetation optical depth product 3

The main goal of the Soil Moisture and Ocean Salinity (SMOS) mission over land surfaces 15 is the production of global maps of soil moisture (SM) and vegetation optical depth (τ) based on 16 multi-angular brightness temperature (TB) measurements at L-band. The operational SMOS Level 17 2 and Level 3 soil moisture algorithms account for different surface effects, such as vegetation 18 opacity an...

متن کامل

Soil moisture retrieval from space: the Soil Moisture and Ocean Salinity (SMOS) mission

Microwave radiometry at low frequencies (L-band: 1.4 GHz, 21 cm) is an established technique for estimating surface soil moisture and sea surface salinity with a suitable sensitivity. However, from space, large antennas (several meters) are required to achieve an adequate spatial resolution at L-band. So as to reduce the problem of putting into orbit a large filled antenna, the possibility of u...

متن کامل

A Novel Bias Correction Method for Soil Moisture and Ocean Salinity (SMOS) Soil Moisture: Retrieval Ensembles

Bias correction is a very important pre-processing step in satellite data assimilation analysis, as data assimilation itself cannot circumvent satellite biases. We introduce a retrieval algorithm-specific and spatially heterogeneous Instantaneous Field of View (IFOV) bias correction method for Soil Moisture and Ocean Salinity (SMOS) soil moisture. To the best of our knowledge, this is the first...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

ژورنال

عنوان ژورنال: Remote Sensing

سال: 2022

ISSN: ['2315-4632', '2315-4675']

DOI: https://doi.org/10.3390/rs14030746