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  4. Tree-ring hydrological research in the Himalaya: State of the art and future directions
 
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Titre

Tree-ring hydrological research in the Himalaya: State of the art and future directions

Type
article
Institution
UNIL/CHUV/Unisanté + institutions partenaires
Périodique
Progress in Physical Geography  
Auteur(s)
Islam, Nazimul
Auteure/Auteur
Vennemann, Torsten
Auteure/Auteur
Büntgen, Ulf
Auteure/Auteur
Cherubini, Paolo
Auteure/Auteur
Lane, Stuart N
Auteure/Auteur
Liens vers les personnes
Vennemann, Torsten  
Lane, Stuart  
Islam, Nazimul  
Liens vers les unités
Inst. dynamiques surface terre  
ISSN
0309-1333
Statut éditorial
Publié
Date de publication
2024-06
Volume
48
Numéro
3
Première page
454
Dernière page/numéro d’article
489
Peer-reviewed
Oui
Langue
anglais
Résumé
Recent developments in tree-ring research offer great potential for reconstructing past climate changes; determining the frequencies of natural hazards; and assessing the availability of freshwater resources over timescales that extend well into the pre-instrumental period. Here, we review the state of dendrochronological research in the Himalaya and outline future directions for tree-ring-based hydrological reconstructions in a region that has a pressing societal need to understand the causes and consequences of past, present and future changes in the hydrological cycle. We used ‘tree ring’ and ‘Himalaya’ as keywords to identify scholarly articles from the Web of Science that were published between 1994 and 2022. The resulting 173 publications were separated by their spatial coverage into the western, central and eastern Himalaya, as well as their scientific purpose (e.g. reconstructing growth-climate relationships, temperature, precipitation, streamflow, floods, droughts, etc.). Our analysis shows that dendrochronological research in the Himalaya primarily focused on understanding growth-climate relationships using annual tree-ring widths measurements obtained for coniferous species, and their application in climate reconstructions. Reconstructions of hydrological processes such as streamflows, and extremes such as glacial and landslide lake outburst floods, have received less attention. Recent advances in dendrochronology, including blue intensity (BI), quantitative wood anatomy (QWA), and tree-ring stable isotopes (TRSI) should be combined to improve the resolution and accuracy of hydrological reconstructions in all parts of the Himalaya. Such studies may allow us to better understand the effects of climate change and the Himalayan water resources for its lowland surroundings. They may also facilitate decision-making processes for mitigating the impacts of climate change on natural hazards, and for better managing water resources in the region.
Sujets

Dendrochronology

tree rings

stable isotopes

quantitative wood ana...

blue intensity

hydrological reconstr...

natural hazard recons...

Himalaya

PID Serval
serval:BIB_6BF0747C1D59
DOI
10.1177/03091333241229919
WOS
001165509100001
Permalien
https://iris.unil.ch/handle/iris/162282
Open Access
Oui
Date de création
2024-07-17T12:17:48.697Z
Date de création dans IRIS
2025-05-20T23:26:14Z
Fichier(s)
En cours de chargement...
Vignette d'image
Nom

Islam et al.2024-Tree-ring hydrology in Himalaya.pdf

Version du manuscrit

published

Licence

https://creativecommons.org/licenses/by/4.0

Taille

1.83 MB

Format

Adobe PDF

PID Serval

serval:BIB_6BF0747C1D59.P001

URN

urn:nbn:ch:serval-BIB_6BF0747C1D595

Somme de contrôle

(MD5):222b1d0724e2403ee90202f69150ebdf

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