SwePub
Sök i LIBRIS databas

  Utökad sökning

id:"swepub:oai:gup.ub.gu.se/327565"
 

Sökning: id:"swepub:oai:gup.ub.gu.se/327565" > Runoff Response to ...

Runoff Response to Climate in Two River Basins Supplied by Small Glacier Meltwater in Southern and Northern Tibetan Plateau

Yao, Ruzhen (författare)
Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences
Li, S. H. (författare)
Chen, Deliang, 1961 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences
 (creator_code:org_t)
2023
2023
Engelska.
Ingår i: Atmosphere. - 2073-4433. ; 14:4
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • The Tibetan Plateau (TP) has experienced amplified warming in recent decades, causing glaciers to melt and affecting river runoff. It is well established that the southern and northern areas of the TP have responded to climate changes differently, with the north dominated by a westerly climate and the south by the Indian monsoon. While there are more glaciers in the TP than in any other region outside the polar areas, most of these glaciers are tiny, and only a limited number of them have been monitored to study mass balance and downward runoff. This study used the mass balance measured at two glaciers along with in situ and satellite data to drive a hydrological model called the Alpine Runoff Predictor that includes glacier melt to simulate glacial melting and the accompanying hydrological processes of the two glacierized basins, analyze their contributions to the river runoffs, and investigate their responses to local climate changes. The results show that the glacier meltwater in both river basins showed an increasing trend, with values of 0.001 x 10(8) m(3) a(-1) in the Kyanjing River basin and 0.0095 x 10(8) m(3) a(-1) in the Tuole River basin. However, their multi-year average contributions to the runoff were 12.5% and 5.6%, respectively. In contrast to the Tuole River basin, where runoff is increasing (0.0617 x 10(8) m(3) a(-1)), the Kyanjing River basin has decreasing runoff (-0.0216 x 10(8) m(3) a(-1)) as a result of decreasing precipitation. This result highlights the dominant role played by precipitation changes in the two basins under study, which are characterized by small glacier meltwater contributions.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)

Nyckelord

runoff
Kyanjing River basin
Tuole River basin
Yala Glacier
Qiyi
Glacier
hydrological response
ice thickness
mass balances
yala glacier
melt
temperature
streamflow
inventory
upstream
products
Environmental Sciences & Ecology
Meteorology & Atmospheric Sciences

Publikations- och innehållstyp

ref (ämneskategori)
art (ämneskategori)

Hitta via bibliotek

Till lärosätets databas

Hitta mer i SwePub

Av författaren/redakt...
Yao, Ruzhen
Li, S. H.
Chen, Deliang, 1 ...
Om ämnet
NATURVETENSKAP
NATURVETENSKAP
och Geovetenskap och ...
NATURVETENSKAP
NATURVETENSKAP
och Geovetenskap och ...
och Meteorologi och ...
Artiklar i publikationen
Atmosphere
Av lärosätet
Göteborgs universitet

Sök utanför SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy