4.3 Article

Evolution properties between meteorological, agricultural and hydrological droughts and their related driving factors in the Luanhe River basin, China

Journal

HYDROLOGY RESEARCH
Volume 50, Issue 4, Pages 1096-1119

Publisher

IWA PUBLISHING
DOI: 10.2166/nh.2019.141

Keywords

agricultural drought; driving factors; hydrological drought; meteorological drought; propagation time

Funding

  1. Natural Science Foundation of China [51579169, 51279123, 51179117]
  2. National Key R & D Program of China [2016YFC0401407]

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To fully reveal drought propagation mechanism and effectively mitigate drought, it is of importance to synthesize investigating different types of droughts; specifically, the propagation from meteorological to agricultural droughts and from agricultural to hydrological droughts, as well as their potential driving factors. The results suggested that: (1) the Standardized Precipitation Evapotranspiration Index (SPEI) is a better indicator for detecting drought onset, the Standardized Soil Index (SSI) can better describe drought persistence, and the Standardized Runoff Index (SRI) can depict the termination of drought; (2) the propagation time from meteorological to agricultural droughts, as well as that from agricultural to hydrological droughts, showed remarkable seasonal characteristics in the Luanhe River basin; (3) the significant influence of the Nino 1+2+3+4, Nino 3.4, Southern Oscillation Index (SOI), Multivariate ENSO Index (MEI), and Atlantic Multidecadal Oscillation (AOM) on meteorological drought was concentrated in the 16-88-month periods, as well as the decadal scale of 99-164-month periods, the significant influence of Nino 4, Nino 3.4, MEI, and SOI on agricultural drought was concentrated in the 16-99-month periods, as well as the decadal scale of 99-187-month periods, and the significant influence of Nino 4 and AOM on hydrological drought was concentrated in the 16-64-month periods, as well as the decadal scale of 104-177-month periods.

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