Jordan Christian - November 6

School of Meteorology Colloquium Flash Droughts: A Local to Global Analysis of Rapid Drought Intensification and their Associated Impacts Jordan Christian   Friday, November 6th 2:00pm Central Time (US and Canada)   Join Zoom Meeting https://oklahoma.zoom.us/j/94939613708?pwd=b00wcy9YajRtRXB5bzcxcC9UL0djUT09 Meeting ID: 949 3961 3708 Passcode: 02824954 Flash drought is characterized by the rapid intensification

Start

November 6, 2020 - 2:00 pm

End

November 6, 2020 - 3:00 pm

School of Meteorology Colloquium

Flash Droughts: A Local to Global Analysis of Rapid Drought Intensification and their Associated Impacts

Jordan Christian

 

Friday, November 6th

2:00pm Central Time (US and Canada)

 

Join Zoom Meeting

https://oklahoma.zoom.us/j/94939613708?pwd=b00wcy9YajRtRXB5bzcxcC9UL0djUT09

Meeting ID: 949 3961 3708

Passcode: 02824954

Flash drought is characterized by the rapid intensification toward drought conditions and is primarily associated with detrimental impacts to agricultural production. Unlike conventional (slowly developing) drought, flash drought can rapidly desiccate land surface conditions in only the span of a few weeks and place excessive stress on the environment. Flash droughts form from a complex combination of thermal, moisture, and radiative flux variables, and predictability of these events remains a significant challenge due to their occurrence on subseasonal timescales. To address some of the challenges related to flash drought development and their associated impacts, the primary goals of this study were to develop an objective methodology for flash drought identification, explore the role of flash drought in socio-economic impacts, and create a global climatology of flash drought occurrence.

 

A comprehensive methodology was developed in conjunction with the standardized evaporative stress ratio (SESR; the ratio between evapotranspiration and potential evapotranspiration) for flash drought identification. After evaluation with the satellite-derived evaporative stress index and U.S. Drought Monitor, a climatology of flash drought events and their characteristics were quantified across the United States. In addition, a case study of a flash drought event over southwestern Russia in 2010 was investigated. It was found that rapid drought development lead to land surface desiccation that primed the land-atmosphere interactions necessary to supplement excessive surface temperatures experienced during a heatwave event. Further, the hydrometeorological extremes associated with the flash drought event resulted in cascading impacts that severely affected ecosystems, agriculture, and human health. Lastly, global hotspots of flash drought occurrence were identified, and several study regions exhibited statistically significant changes in flash drought spatial coverage between 1980 and 2015.

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