2021
DOI: 10.1061/(asce)he.1943-5584.0002039
|View full text |Cite
|
Sign up to set email alerts
|

Nonstationary Modeling of Meteorological Droughts: Application to a Region in India

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1

Citation Types

0
4
0

Year Published

2021
2021
2024
2024

Publication Types

Select...
4
3

Relationship

1
6

Authors

Journals

citations
Cited by 25 publications
(4 citation statements)
references
References 103 publications
0
4
0
Order By: Relevance
“…The non-stationary version of different indices is obtained by incorporating additional covariates and employing regression analysis to estimate the corresponding positional parameters. The mainstream calculation method uses time or circulation index as covariates [44,45]. There are also alternative options for covariates, with human activity being one possible choice [46].…”
Section: Non-stationary Input Variables Of the Drought Indexmentioning
confidence: 99%
“…The non-stationary version of different indices is obtained by incorporating additional covariates and employing regression analysis to estimate the corresponding positional parameters. The mainstream calculation method uses time or circulation index as covariates [44,45]. There are also alternative options for covariates, with human activity being one possible choice [46].…”
Section: Non-stationary Input Variables Of the Drought Indexmentioning
confidence: 99%
“…Traditionally droughts and heatwaves have been studied separately to assess the risk associated with them (Das et al, 2022a; Das, Das, & Umamahesh, 2021; Perkins‐Kirkpatrick & Lewis, 2020; Shao et al, 2018). Studies on droughts and hot events around the world have shown, that over time the vulnerabilities of both events are growing in most regions (Campbell et al, 2018; McMichael & Lindgren, 2011).…”
Section: Introductionmentioning
confidence: 99%
“…The studies, as mentioned above, except a few, employed Standardized Precipitation Index (SPI) as a meteorological drought indicator to characterize the drought under the future climate change scenarios. According to the definition, SPI accounts only precipitation to describe the drought (Mckee et al ., 1993; Das et al ., 2021). However, in the present climate change scenario, it is expected that with constant relative humidity, the moisture content in the atmosphere roughly increases by 6–7% K −1 rise in the lower tropospheric temperature (Willett et al ., 2007).…”
Section: Introductionmentioning
confidence: 99%