Developing a drought-monitoring index for the contiguous US using SMAP

Sara Sadri, Eric F. Wood, Ming Pan
2018 Hydrology and Earth System Sciences  
<p><strong>Abstract.</strong> Since April 2015, NASA's Soil Moisture Active Passive (SMAP) mission has monitored near-surface soil moisture, mapping the globe (between 85.044<span class="inline-formula"><sup>∘</sup></span><span class="thinspace"></span>N/S) using an L-band (1.4<span class="thinspace"></span>GHz) microwave radiometer in 2–3 days depending on location. Of particular interest to SMAP-based agricultural applications is a monitoring product that assesses the SMAP near-surface soil
more » ... isture in terms of probability percentiles for dry and wet conditions. However, the short SMAP record length poses a statistical challenge for meaningful assessment of its indices. This study presents initial insights about using SMAP for monitoring drought and pluvial regions with a first application over the contiguous United States (CONUS). SMAP soil moisture data from April 2015 to December 2017 at both near-surface (5<span class="thinspace"></span>cm) SPL3SMP, or Level 3, at <span class="inline-formula">∼36</span><span class="thinspace"></span>km resolution, and root-zone SPL4SMAU, or Level 4, at <span class="inline-formula">∼9</span><span class="thinspace"></span>km resolution, were fitted to beta distributions and were used to construct probability distributions for warm (May–October) and cold (November–April) seasons. To assess the data adequacy and have confidence in using short-term SMAP for a drought index estimate, we analyzed individual grids by defining two filters and a combination of them, which could separate the 5815 grids covering CONUS into passed and failed grids. The two filters were (1) the Kolmogorov–Smirnov (KS) test for beta-fitted long-term and the short-term variable infiltration capacity (VIC) land surface model (LSM) with 95<span class="thinspace"></span>% confidence and (2) good correlation (<span class="inline-formula">≥0.4</span>) between beta-fitted VIC and beta-fitted SPL3SMP. To evaluate which filter is the best, we defined a mean distance (MD) metric, assuming a VIC index at 36<span class="thinspace"></span>km resolution as the ground truth. For both warm and cold seasons, the union of the filters – which also gives the best coverage of the grids throughout CONUS – was chosen to be the most reliable filter. We visually compared our SMAP-based drought index maps with metrics such as the U.S. Drought Monitor (from D0–D4), 1-month Standard Precipitation Index (SPI) and near-surface VIC from Princeton University. The root-zone drought index maps were shown to be similar to those produced by the root-zone VIC, 3-month SPI, and the Gravity Recovery and Climate Experiment (GRACE). This study is a step forward towards building a national and international soil moisture monitoring system without which quantitative measures of drought and pluvial conditions will remain difficult to judge.</p>
doi:10.5194/hess-22-6611-2018 fatcat:etukaykvljd3jp66e7htoex66e