EGU2020-14871, updated on 12 Jun 2020
https://doi.org/10.5194/egusphere-egu2020-14871
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Operational Near-real Time Drought Monitoring Using Global Satellite Precipitation Estimates

Olivier Prat1, Alec Courtright2, Ronald Leeper1, Brian Nelson3, Rocky Bilotta2, James Adams4, and Steve Ansari5
Olivier Prat et al.
  • 1Cooperative Institute for Satellite Earth System Studies (CISESS), North Carolina State University, Asheville, NC, USA (opprat@ncsu.edu)
  • 2ISciences, National Centers for Environmental Information (NCEI), Asheville, NC, USA
  • 3NOAA/NCEI/Center for Weather and Climate (CWC), Asheville, NC, USA
  • 4Formerly of ERT/NCEI, Asheville, NC
  • 5NOAA/NCEI/National Integrated Drought Information System (NIDIS), Asheville, NC, USA

We present an operational near-real time drought monitoring framework on a global scale that uses satellite quantitative precipitation estimates from the NOAA/CDR program (CMORPH-CDR, PERSIANN-CDR). Monthly and daily Standardized Precipitation Indexes (SPI) are computed for various time scales over the entire period of record of the respective datasets. The near-real time availability of CMORPH-CDR permits for a daily update of the global drought conditions starting in 1998, while the longer period of record of PERSIANN-CDR allows to compute global drought conditions since 1983. The SPI sensitivity to different precipitation datasets and to various lengths of record is quantified. Results indicated that both monthly and daily SPIs computed with both CDRs presented the same timing and area for the major droughts episodes over the continental United States as well as for selected drought events around the globe. Furthermore, the difference resulting from the use of the two-parameter Gamma distribution (McKee et al. 1993) and the three-parameter Pearson III distribution (Guttman 1999) is evaluated. The global mapping of the different distribution parameters (2 and 3 parameters respectively for the Gamma and Pearson III distributions) informs us on how to optimally compute the SPI in areas experiencing too much or too little rainfall. Both CMORPH-CDR and PERSIANN-CDR SPIs are evaluated primarily over CONUS where long-term drought monitoring products based on in-situ data exists such as the United States Drought Monitor (USDM) and the nClimGrid derived SPI. A publicly available interactive visualization tool that provides access to global drought information is also presented. The tools is intended to fill some of the drought monitoring information gaps around the globe. A variety of visualization techniques are used to aid in the interpretation of global drought indices while interactive functionality allows users to focus on a specific region and time-scale of interest. Additional information for region specific drought monitoring resources is also provided to help users access regional drought monitoring information.

How to cite: Prat, O., Courtright, A., Leeper, R., Nelson, B., Bilotta, R., Adams, J., and Ansari, S.: Operational Near-real Time Drought Monitoring Using Global Satellite Precipitation Estimates , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-14871, https://doi.org/10.5194/egusphere-egu2020-14871, 2020

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