吉尔吉特盆地温度变化背景下的降雪评价

A. Shehzadi, Syed Amer Mehmood, H. Aeman, S. Batool
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引用次数: 0

摘要

以吉尔吉特河和罕萨河流域为研究对象,开展了吉尔吉特河流域气温变化背景下的积雪评价研究。该流域的低空曲线在归一化面积和海拔之间呈凸向上。利用MODIS积雪产品对流域积雪进行分类。变化检测技术表明,2011年融化期积雪面积变化幅度较大。2011年融雪期融雪面积为9358.762km2。吉尔吉特—罕萨河在2011年、2012年和2015年融化期出现了高水平的积雪变化检测。融化期积雪面积变化最小的年份是2014年。在这一年中,观测到融雪,变化检测水平较低。此外,2013年融化期的积雪变化检测水平也较低。该流域积雪变化呈减小趋势。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
APPRAISAL OF SNOW IN CONTEXT OF TEMPERATURE VARIATIONS IN GILGIT BASIN
The study on Appraisal of Snow in Context of Temperature Variations in Gilgit Basin was conducted to find the snow cover change over Gilgit and Hunza Rivers. Hypsometric curve for this catchment was convex upward between normalized area and elevation. Using the MODIS snow cover product classification of snow cover was done which indicate the present of snow in the catchment. Change detection technique indicates there was high level of snow cover area change during the melting period of 2011. This area of snow which melted during melting period of 2011 was 9358.762km2. There was high level of snow cover change detection appeared in the melting period of 2011, 2012 and 2015 along the Gilgit-Hunza Rivers. The minimum snow area change was observed in 2014 during the melting period. During this year snow melting was observed with low level of change detection. Besides there was also low level of snow cover change detection observed in 2013 melting period. There was decreasing trend in snow cover change appeared in this basin.
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