Development of Agricultural Drought Assessment Approach Using SMAP Soil Moisture Footprints
2017
Shin, Y., Kyungpook National University, Daegu, Republic of Korea | Lee, T., Kyungpook National University, Daegu, Republic of Korea | Kim, S., Kyungpook National University, Daegu, Republic of Korea | Lee, H.W., Kyungpook National University, Daegu, Republic of Korea | Choi, K.S., Kyungpook National University, Daegu, Republic of Korea | Kim, J., Kangwon National University, Chuncheon, Republic of Korea | Lee, G., Kyungpook National University, Daegu, Republic of Korea
In this study, we evaluated daily root zone soil moisture dynamics and agricultural drought using a near-surface soil moisture data assimilation scheme with Soil Moisture Active & Passive (SMAP, 3 km x 3 km) soil moisture footprints under different hydro-climate conditions. Satellite-based LANDSAT and MODIS image footprints were converted to spatially-distributed soil moisture estimates based on the regression model, and the converted soil moisture distributions were used for assessing uncertainties and applicability of SMAP data at fields. In order to overcome drawbacks of the discontinuity of SMAP data at the spatio-temporal scales, the data assimilation was applied to SMAP for estimating daily soil moisture dynamics at the spatial domain. Then, daily soil moisture values were used to estimate weekly agricultural drought based on the Soil Moisture Deficit Index (SMDI). The Yongdam-dam and Soyan river-dam watersheds were selected for validating our proposed approach. As a results, the MODIS/SMAP soil moisture values were relatively overestimated compared to those of the TDR-based measurements and LANDSAT data. When we applied the data assimilation scheme to SMAP, uncertainties were highly reduced compared to the TDR measurements. The estimated daily root zone soil moisture dynamics and agricultural drought from SMAP showed the variability at the sptio-temporal scales indicating that soil moisture values are influenced by not only the precipitation, but also the land surface characteristics. These findings can be useful for establishing efficient water management plans in hydrology and agricultural drought.
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