Hydro-climatological Extremes
Hydrological Hazard
Multivariate Hydrological Analysis
Detection and Attribution of Extreme Events
Regional Hydrological Modelling
Water Accounting
Climate and Ecological Resilience
Meteorological drought is the initial stage of drought, and the prolonged duration of meteorological drought leads to agricultural, hydrological, and socio-economic droughts. The major hydrological component which causes meteorological drought is rainfall. One of the familiar indices used to extract meteorological drought characteristics is the standard precipitation index (SPI), which is developed on the basic assumption of stationary (i.e., the statistical properties do not change over time) climate. However, numerous studies proved that the statistical properties of precipitation have changed. Hence, the stationary assumption used in SPI is no longer reliable and cannot trace the changing characteristics of drought. Recently more attention is given to the development of a nonstationary drought index. The major drawback of the nonstationary drought index is the uncertainty about future prediction and the lack of knowledge about the physical processes (Climate-informed covariates) behind the changes. Moreover, the spatio-temporal evolution of meteorological drought over India is still not established. Hence, this study aims to understand the cause and effect of meteorological drought and re-examine the meteorological drought severity trend by extracting the drought characteristics using a nonstationary drought index. The following objectives are formulated to achieve this goal:
Interns will be introduced to the new research world of non-stationarity. By the end of this internship, the student will be well versed in programming language and stochastic hydrology.
Room No. 228
Department of Civil Engineering
Indian Institute of Technology Roorkee
Roorkee - 247667
Haridwar District, Uttarakhand
vinnarasi@ce.iitr.ac.in