Assimilation of SMAP Brightness Temperature Observations in the GEOS Land–Atmosphere Data Assimilation System

oleh: Rolf H. Reichle, Sara Q. Zhang, Qing Liu, Clara S. Draper, Jana Kolassa, Ricardo Todling

Format: Article
Diterbitkan: IEEE 2021-01-01

Deskripsi

Errors in soil moisture adversely impact the modeling of land&#x2013;atmosphere water and energy fluxes and, consequently, near-surface atmospheric conditions in atmospheric data assimilation systems (ADAS). To mitigate such errors, a land surface analysis is included in many such systems, although not yet in the currently operational NASA Goddard Earth Observing System (GEOS) ADAS. This article investigates the assimilation of L-band brightness temperature (Tb) observations from the Soil Moisture Active Passive (SMAP) mission in the GEOS weakly coupled land&#x2013;atmosphere data assimilation system (LADAS) during boreal summer 2017. The SMAP Tb analysis improves the correlation of LADAS surface and root-zone soil moisture versus <italic>in situ</italic> measurements by &#x223C;0.1&#x2013;0.26 over that of ADAS estimates; the unbiased root-mean-square error of LADAS soil moisture is reduced by 0.002&#x2013;0.008 m<sup>3</sup>&#x002F;m<sup>3</sup> from that of ADAS. Furthermore, the global land average RMSE versus <italic>in situ</italic> measurements of screen-level air specific humidity (q2m) and daily maximum temperature (T2m<sub>max</sub>) is reduced by 0.05 g&#x002F;kg and 0.04 K, respectively, for LADAS compared to ADAS estimates. Regionally, the RMSE of LADAS q2m and T2m<sub>max</sub> is improved by up to 0.4 g&#x002F;kg and 0.3 K, respectively. Improvement in LADAS specific humidity extends into the lower troposphere (below &#x223C;700 mb), with relative improvements in bias of 15&#x2013;25&#x0025;, although LADAS air temperature bias slightly increases relative to that of ADAS. Finally, the root mean square of the LADAS Tb observation-minus-forecast residuals is smaller by up to &#x223C;0.1 K than in a land-only assimilation system, corroborating the positive impact of the Tb analysis on the modeled land&#x2013;atmosphere coupling.