کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6413704 1629953 2013 14 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Integrated flow and temperature modeling at the catchment scale
ترجمه فارسی عنوان
مدل سازی مجدد جریان و درجه حرارت در مقیاس حوضه
کلمات کلیدی
دمای جریان، مدل سازی آبهای زیرزمینی آب یکپارچه، آیداهو، نقره کریک،
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی


- We developed a surface water-groundwater flow and heat model for basin management.
- Integrated flow dynamics were essential in predicting accurate stream temperature.
- A 10% reduction of groundwater flow causes a mean temperature increase of 0.5 °C.
- The model serves as a valuable tool for ecohydrology assessment in a catchment.

SummaryChanges in natural stream temperature levels can be detrimental to the health of aquatic ecosystems. Water use and land management directly affect the distribution of diffuse heat sources and thermal loads to streams, while riparian vegetation and geomorphology play a critical role in how thermal loads are buffered. In many areas, groundwater flow is a significant contribution to river flow, particularly during low flows and therefore has a strong influence on stream temperature levels and dynamics. However, previous stream temperature models do not properly simulate how surface water-groundwater dynamics affect stream temperature. A coupled surface water-groundwater and temperature model has therefore been developed to quantify the impacts of land management and water use on stream flow and temperatures. The model is applied to the simulation of stream temperature levels in a spring-fed stream, the Silver Creek Basin in Idaho, where stream temperature affects the populations of fish and other aquatic organisms. The model calibration highlights the importance of spatially distributed flow dynamics in the catchment to accurately predict stream temperatures. The results also show the value of including temperature data in an integrated flow model calibration because temperature data provide additional constraints on the flow sources and volumes. Simulations show that a reduction of 10% in the groundwater flow to the Silver Creek Basin can cause average and maximum temperature increases in Silver Creek over 0.3 °C and 1.5 °C, respectively. In spring-fed systems like Silver Creek, it is clearly not feasible to separate river habitat restoration from upstream catchment and groundwater management.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Hydrology - Volume 495, 12 July 2013, Pages 238-251
نویسندگان
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