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

<p>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>&thinsp;N/S) using an L-band (1.4&thinsp;GHz) microw...

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Main Authors: S. Sadri, E. F. Wood, M. Pan
Format: Article
Language:English
Published: Copernicus Publications 2018-12-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/22/6611/2018/hess-22-6611-2018.pdf
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spelling doaj-8c13a56296644919ad054bd5f77539c52020-11-25T01:14:55ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382018-12-01226611662610.5194/hess-22-6611-2018Developing a drought-monitoring index for the contiguous US using SMAPS. Sadri0E. F. Wood1M. Pan2Department of Civil and Environmental Engineering, Princeton University, 59 Olden St, Princeton, NJ 08540, USADepartment of Civil and Environmental Engineering, Princeton University, 59 Olden St, Princeton, NJ 08540, USADepartment of Civil and Environmental Engineering, Princeton University, 59 Olden St, Princeton, NJ 08540, USA<p>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>&thinsp;N/S) using an L-band (1.4&thinsp;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 moisture 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&thinsp;cm) SPL3SMP, or Level 3, at <span class="inline-formula">∼36</span>&thinsp;km resolution, and root-zone SPL4SMAU, or Level 4, at <span class="inline-formula">∼9</span>&thinsp;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&thinsp;% 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&thinsp;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>https://www.hydrol-earth-syst-sci.net/22/6611/2018/hess-22-6611-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. Sadri
E. F. Wood
M. Pan
spellingShingle S. Sadri
E. F. Wood
M. Pan
Developing a drought-monitoring index for the contiguous US using SMAP
Hydrology and Earth System Sciences
author_facet S. Sadri
E. F. Wood
M. Pan
author_sort S. Sadri
title Developing a drought-monitoring index for the contiguous US using SMAP
title_short Developing a drought-monitoring index for the contiguous US using SMAP
title_full Developing a drought-monitoring index for the contiguous US using SMAP
title_fullStr Developing a drought-monitoring index for the contiguous US using SMAP
title_full_unstemmed Developing a drought-monitoring index for the contiguous US using SMAP
title_sort developing a drought-monitoring index for the contiguous us using smap
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2018-12-01
description <p>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>&thinsp;N/S) using an L-band (1.4&thinsp;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 moisture 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&thinsp;cm) SPL3SMP, or Level 3, at <span class="inline-formula">∼36</span>&thinsp;km resolution, and root-zone SPL4SMAU, or Level 4, at <span class="inline-formula">∼9</span>&thinsp;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&thinsp;% 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&thinsp;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>
url https://www.hydrol-earth-syst-sci.net/22/6611/2018/hess-22-6611-2018.pdf
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