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Inter-annual variability in snow cover depletion patterns and atmospheric circulation indices in the Upper Irtysh basin, Central Asia

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dc.contributor.author Fugazza, Davide
dc.contributor.author Shaw, Thomas E.
dc.contributor.author Mashtayeva, Shamshagul
dc.contributor.author Brock, Benjamin
dc.date.accessioned 2024-10-16T07:07:08Z
dc.date.available 2024-10-16T07:07:08Z
dc.date.issued 2020
dc.identifier.issn 08856087
dc.identifier.other DOI 10.1002/hyp.13843
dc.identifier.uri http://rep.enu.kz/handle/enu/17766
dc.description.abstract The Irtysh River is the main water resource of Eastern Kazakhstan and its upper basin is severely affected by spring floods each year, primarily as a result of snowmelt. Knowledge of the large-scale processes that influence the timing of these snow-induced floods is currently lacking, but critical for the management of water resources in the area. In this study, we evaluated the variability in winter–spring snow cover in five major sub-basins of the Upper Irtysh basin between 2000 and 2017 as a possible explanatory factor of spring flood events, assessing the time of peak snow cover depletion rate and snow cover disappearance from the moderate-resolution imaging spectroradiometer (MODIS) MOD10A2 data set. We found that on average, peak snow cover retreat occurs between 22 March and 14 April depending on the basin, with large interannual variations but no clear trend over the MODIS period, while our comparative analysis of longer-term snow cover extent from the National Oceanic and Atmospheric Administration Climate Data Record data set suggests a shift to earlier snow cover disappearance since the 1970s. In contrast, the annual peak snow cover depletion rate displays a weak increasing trend over the study period and exceeded 5,900 km2/day in 2017. The timing of snow disappearance in spring shows significant correlations of up to 0.82 for the largest basin with winter indices of the Arctic Oscillation (AO) over the region. The primary driver is the impact of the large-scale pressure anomalies upon the mean spring (MAM) air temperatures and resultant timing of snow cover disappearance, particularly at elevations 500–2,000 m above sea level. This suggests a lagged effect of this atmospheric circulation pattern in spring snow cover retreat. The winter AO index could therefore be incorporated into long-term runoff forecasts for the Irtysh. Our approach is easily transferable to other similar catchments and could support flood management strategies in Kazakhstan and other countries. ru
dc.language.iso en ru
dc.publisher Hydrological Processes ru
dc.relation.ispartofseries Том 34, Выпуск 18, Страницы 3738 - 3757;
dc.subject Arctic Oscillation ru
dc.subject atmospheric circulation ru
dc.subject MODIS ru
dc.subject Siberian high ru
dc.subject snow cover depletion ru
dc.subject Upper Irtysh River ru
dc.title Inter-annual variability in snow cover depletion patterns and atmospheric circulation indices in the Upper Irtysh basin, Central Asia ru
dc.type Article ru


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