2022
DOI: 10.1007/978-3-030-92782-0_3
|View full text |Cite
|
Sign up to set email alerts
|

Tree-Ring-Based Hydrological Records Reconstructions of the Himalayan Rivers: Challenges and Opportunities

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
3
0

Year Published

2022
2022
2024
2024

Publication Types

Select...
3
1

Relationship

1
3

Authors

Journals

citations
Cited by 4 publications
(3 citation statements)
references
References 102 publications
0
3
0
Order By: Relevance
“…common climatic conditions (mainly precipitation and evapotranspiration), which control tree growth and streamflow reconstruction [46,47].…”
Section: Discussionmentioning
confidence: 99%
“…common climatic conditions (mainly precipitation and evapotranspiration), which control tree growth and streamflow reconstruction [46,47].…”
Section: Discussionmentioning
confidence: 99%
“…The major shifts in climate causing floods and droughts are linked with the rise and fall of civilizations (Kathayat et al, 2017). The potential effect of hydroclimate alterations as a result of a changing global climate creates significant issues in mountainous regions, which are a source of public concern (Tiwari et al, 2018;Valdiya, 2020;Shekhar et al, 2022). The Indian summer monsoon is connected to numerous largescale ocean/atmospheric circulation patterns and is exacerbated under global warming scenarios (Lal, 2003;Kripalani et al, 2007;Lucas-Picher et al, 2011;Menon et al, 2013;Roxy et al, 2015;Huang et al, 2020;Sabin et al, 2020).…”
Section: Introductionmentioning
confidence: 99%
“…To enhance knowledge of the dynamics and causes of monsoon variability in Southeast Asia, several proxies, such as tree rings, ice cores, and speleothems, have been investigated to extend climatic records (Singhvi and Kale, 2010). Tree ring width is a commonly used proxy in the Himalayan regions to reconstruct precipitation and temperature (Bhattacharyya and Yadav, 1999;Singh et al, 2006;Yadav et al, 2011;Shekhar, 2014;Shekhar et al, 2022), relative humidity (Dhyani et al, 2021b), and droughts (Cook et al, 2010;Yadav et al, 2017;Shekhar et al, 2018;Dhyani et al, 2022a). In addition, a gridded spatial reconstruction of the Palmer Drought Severity Index (PDSI) throughout Asia included building the Himalayan drought history (Cook et al, 2010).…”
Section: Introductionmentioning
confidence: 99%