Using microwave brightness temperature diurnal cycle to improve emissivity retrievals over land

REMOTE SENSING OF ENVIRONMENT

卷:123

Article

Norouzi, Hamidreza^1,2  Rossow, William²  Temimi, Marouane²  Prigent, Catherine³  Azarderakhsh, Marzieh²  Boukabara, Sid⁴  Khanbilvardi, Reza² 

[1] CUNY, New York City Coll Technol, Brooklyn, NY 11201 USA

[2] CUNY City Coll, NOAA Cooperat Remote Sensing Sci & Technol Ctr CR, New York, NY 10031 USA

[3] Observ Paris, CNRS, Lab Etud Rayonnement & Matiere Astrophys, F-75014 Paris, France

[4] NOAA, NESDIS, Ctr Satellite Applicat & Res STAR, Camp Springs, MD 20746 USA

关键词: Emissivity;    Brightness temperature;    Diurnal cycle;    Land;    Passive microwave;    Effective temperature;    Vegetation;    Soil moisture;   

DOI  :  10.1016/j.rse.2012.04.015

来源: Elsevier

【 摘 要 】

To retrieve microwave land emissivity, infrared surface skin temperatures have been used as surface physical temperature since there is no global information on physical vegetation/soil temperature profiles. However, passive microwave emissions originate from deeper layers with respect to the skin temperature. So, this inconsistency in sensitivity depths between skin temperatures and microwave temperatures may introduce a discrepancy in the determined emissivity. Previous studies showed that this inconsistency can lead to significant differences between day and night retrievals of land emissivity which can exceed 10%. This study proposes an approach to address this inconsistency and improve the retrieval of land emissivity using microwave observations from Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E). The diurnal cycle of the microwave brightness temperature (Tb) was constructed over the globe for different frequencies/polarizations using a constellation of satellites. Principal component analysis (PCA) was conducted to evaluate the spatial variation of the Tb diurnal cycle. The diurnal amplitudes of microwave temperatures observed in desert areas were not consistent with the larger amplitudes of the diurnal cycle of skin temperature. Densely vegetated areas with more moisture have shown smaller amplitudes. A lookup table of effective temperature (T-eff) anomalies is constructed based on the Tb diurnal cycle to resolve the inconsistencies between infrared and Tb diurnal variation. This lookup table of T-eff anomalies is a weighted average over the layers contributing to the microwave signal, for each channel and month. The integration of this T-eff in the retrieval of land emissivity reduced the differences between day and night retrieved emissivities to less than 0.01 for AMSR-E observations. (C) 2012 Elsevier Inc. All rights reserved.

【 授权许可】

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