Development of a Flash Drought Intensity Index
Flash droughts are characterized by a period of rapid intensification over sub-seasonal time scales that culminates in the rapid emergence of new or worsening drought impacts. This study presents a new flash drought intensity index (FDII) that accounts for both the unusually rapid rate of drought in...
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doaj-0f805089e6e04adc821df09fc0e2dd7b2021-06-30T23:41:29ZengMDPI AGAtmosphere2073-44332021-06-011274174110.3390/atmos12060741Development of a Flash Drought Intensity IndexJason A. Otkin0Yafang Zhong1Eric D. Hunt2Jordan I. Christian3Jeffrey B. Basara4Hanh Nguyen5Matthew C. Wheeler6Trent W. Ford7Andrew Hoell8Mark Svoboda9Martha C. Anderson10Space Science and Engineering Center, Cooperative Institute for Meteorological Satellite Studies, University of Wisconsin-Madison, Madison, WI 53706, USASpace Science and Engineering Center, Cooperative Institute for Meteorological Satellite Studies, University of Wisconsin-Madison, Madison, WI 53706, USAAtmospheric and Environmental Research, Inc., Lexington, MA 02421, USASchool of Meteorology, University of Oklahoma, Norman, OK 73702, USASchool of Meteorology, University of Oklahoma, Norman, OK 73702, USABureau of Meteorology, Melbourne, VIC 3008, AustraliaBureau of Meteorology, Melbourne, VIC 3008, AustraliaIllinois Water Survey, University of Illinois, Champaign, IL 61820, USAPhysical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO 80305, USANational Drought Mitigation Center, University of Nebraska, Lincoln, NE 68583, USAAgricultural Research Service, Hydrology and Remote Sensing Laboratory, United States Department of Agriculture, Beltsville, MD 20705, USAFlash droughts are characterized by a period of rapid intensification over sub-seasonal time scales that culminates in the rapid emergence of new or worsening drought impacts. This study presents a new flash drought intensity index (FDII) that accounts for both the unusually rapid rate of drought intensification and its resultant severity. The FDII framework advances our ability to characterize flash drought because it provides a more complete measure of flash drought intensity than existing classification methods that only consider the rate of intensification. The FDII is computed using two terms measuring the maximum rate of intensification (FD_INT) and average drought severity (DRO_SEV). A climatological analysis using soil moisture data from the Noah land surface model from 1979–2017 revealed large regional and interannual variability in the spatial extent and intensity of soil moisture flash drought across the US. Overall, DRO_SEV is slightly larger over the western and central US where droughts tend to last longer and FD_INT is ~75% larger across the eastern US where soil moisture variability is greater. Comparison of the FD_INT and DRO_SEV terms showed that they are strongly correlated (r = 0.82 to 0.90) at regional scales, which indicates that the subsequent drought severity is closely related to the magnitude of the rapid intensification preceding it. Analysis of the 2012 US flash drought showed that the FDII depiction of severe drought conditions aligned more closely with regions containing poor crop conditions and large yield losses than that captured by the intensification rate component (FD_INT) alone.https://www.mdpi.com/2073-4433/12/6/741flash droughtdroughtsoil moisturecrop yieldclimateclimate extreme |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Jason A. Otkin Yafang Zhong Eric D. Hunt Jordan I. Christian Jeffrey B. Basara Hanh Nguyen Matthew C. Wheeler Trent W. Ford Andrew Hoell Mark Svoboda Martha C. Anderson |
spellingShingle |
Jason A. Otkin Yafang Zhong Eric D. Hunt Jordan I. Christian Jeffrey B. Basara Hanh Nguyen Matthew C. Wheeler Trent W. Ford Andrew Hoell Mark Svoboda Martha C. Anderson Development of a Flash Drought Intensity Index Atmosphere flash drought drought soil moisture crop yield climate climate extreme |
author_facet |
Jason A. Otkin Yafang Zhong Eric D. Hunt Jordan I. Christian Jeffrey B. Basara Hanh Nguyen Matthew C. Wheeler Trent W. Ford Andrew Hoell Mark Svoboda Martha C. Anderson |
author_sort |
Jason A. Otkin |
title |
Development of a Flash Drought Intensity Index |
title_short |
Development of a Flash Drought Intensity Index |
title_full |
Development of a Flash Drought Intensity Index |
title_fullStr |
Development of a Flash Drought Intensity Index |
title_full_unstemmed |
Development of a Flash Drought Intensity Index |
title_sort |
development of a flash drought intensity index |
publisher |
MDPI AG |
series |
Atmosphere |
issn |
2073-4433 |
publishDate |
2021-06-01 |
description |
Flash droughts are characterized by a period of rapid intensification over sub-seasonal time scales that culminates in the rapid emergence of new or worsening drought impacts. This study presents a new flash drought intensity index (FDII) that accounts for both the unusually rapid rate of drought intensification and its resultant severity. The FDII framework advances our ability to characterize flash drought because it provides a more complete measure of flash drought intensity than existing classification methods that only consider the rate of intensification. The FDII is computed using two terms measuring the maximum rate of intensification (FD_INT) and average drought severity (DRO_SEV). A climatological analysis using soil moisture data from the Noah land surface model from 1979–2017 revealed large regional and interannual variability in the spatial extent and intensity of soil moisture flash drought across the US. Overall, DRO_SEV is slightly larger over the western and central US where droughts tend to last longer and FD_INT is ~75% larger across the eastern US where soil moisture variability is greater. Comparison of the FD_INT and DRO_SEV terms showed that they are strongly correlated (r = 0.82 to 0.90) at regional scales, which indicates that the subsequent drought severity is closely related to the magnitude of the rapid intensification preceding it. Analysis of the 2012 US flash drought showed that the FDII depiction of severe drought conditions aligned more closely with regions containing poor crop conditions and large yield losses than that captured by the intensification rate component (FD_INT) alone. |
topic |
flash drought drought soil moisture crop yield climate climate extreme |
url |
https://www.mdpi.com/2073-4433/12/6/741 |
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