DC pole | Wartość | Język |
dc.contributor.author | Chen, Feng | - |
dc.contributor.author | Opala-Owczarek, Magdalena | - |
dc.contributor.author | Khan, Adam | - |
dc.contributor.author | Zhang, Heli | - |
dc.contributor.author | Owczarek, Piotr | - |
dc.contributor.author | Chen, Youping | - |
dc.contributor.author | Ahmed, Moinuddin | - |
dc.contributor.author | Chen, Fahu | - |
dc.date.accessioned | 2021-09-24T10:08:17Z | - |
dc.date.available | 2021-09-24T10:08:17Z | - |
dc.date.issued | 2021 | - |
dc.identifier.citation | "Environmental Research Letters", 2021, no. 9, art. no. 094055, s. 1-13 | pl_PL |
dc.identifier.issn | 1748-9326 | - |
dc.identifier.uri | http://hdl.handle.net/20.500.12128/21639 | - |
dc.description.abstract | Given the reported increasing trends in high Asian streamflow and rapidly increasing water
demand in the Indian subcontinent, it is necessary to understand the long-term changes and
mechanisms of snow- and glacier-melt-driven streamflow in this area. Thus, we have developed a
June–July streamflow reconstruction for the upper Indus River watershed located in northern
Pakistan. This reconstruction used a temperature-sensitive tree-ring width chronology of Pinus
wallichiana, and explained 40.9% of the actual June–July streamflow variance during the common
period 1970–2008. The high level of streamflow (1990–2017) exceeds that of any other time and is
concurrent with the impact of recent climate warming that has resulted in accelerated glacier
retreats across high Asia. The streamflow reconstruction indicated a pronounced reduction in
streamflow in the upper Indus River basin during solar minima (Maunder, Dalton, and Damon).
Shorter periods (years) of low streamflow in the reconstruction corresponded to major volcanic
eruptions. Extreme low and high streamflows were also linked with sea surface temperature. The
streamflow reconstruction also provides a long-term context for recent high Asian streamflow
variability resulting from seasonal snow and glaciers that is critically needed for water resources
management and assessment. | pl_PL |
dc.language.iso | en | pl_PL |
dc.rights | Uznanie autorstwa 3.0 Polska | * |
dc.rights.uri | http://creativecommons.org/licenses/by/3.0/pl/ | * |
dc.subject | upper Indus River | pl_PL |
dc.subject | high Asia | pl_PL |
dc.subject | tree rings | pl_PL |
dc.subject | streamflow reconstruction | pl_PL |
dc.subject | volcanic eruption | pl_PL |
dc.subject | solar activity | pl_PL |
dc.title | Late twentieth century rapid increase in high Asian seasonal snow and glacierderived streamflow tracked by tree rings of the upper Indus River basin | pl_PL |
dc.type | info:eu-repo/semantics/article | pl_PL |
dc.identifier.doi | 10.1088/1748-9326/ac1b5c | - |
Pojawia się w kolekcji: | Artykuły (WNP)
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