کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6303276 1618237 2015 15 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Mountain-river runoff components and their role in the seasonal development of desert-oases in northwest China
ترجمه فارسی عنوان
اجزای روان کوهستانی رودخانه و نقش آنها در توسعه فصلی نواحی بیابانی در شمال غربی چین
کلمات کلیدی
چرخه هیدرولوژیکی، اندازه گیری های هیدرومتری، رابطه رطوبت-رواناب، سنجش از دور، محاسبات آب تعادل،
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی
The paper examines the role of mountain runoff in the seasonal growth of oasis vegetation in the hyper-arid region of northwest China. Central to this examination is the development of a simple hydrologic model that relates hydrologic inflows and outflows estimated from remote sensing data (e.g., evapotranspiration, precipitation, snow accumulation, and snowmelt) to the calculation of runoff over a ten-year period (2000-2009). Modeled runoff is shown to reproduce the seasonal trends in hydrometric data fairly well, yielding R2's of 0.75 and 0.66 for stations in the upper reaches of the Shiyang and Hei River systems. Greater than 90% of the runoff from the Qilian Mountains to the oases occurs during the May-September period. Considerable discrepancy between modeled and observed runoff exists in the lower reaches of the rivers, where significant amounts of river water (>45%) are routinely extracted for cropland irrigation. Along the river systems, where water extraction and inflow of glacial meltwater are minor, model calculations replicate observed water yields much more closely. Analysis of seasonal trends in the contribution of snowmelt and rainfall to the return flow, reveals snowmelt as having the greatest influence in initiating the oasis growing period during the March-to-May period of each year.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Arid Environments - Volume 122, November 2015, Pages 1-15
نویسندگان
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