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Review of Statistical Water Temperature Models for a Peruvian Andean River
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作者 Efrain Noa-Yarasca Diana Chaca Ayuque +2 位作者 Hugo A.Galvan Ccora Ivan A.Ayala Bizarro Ada Arancibia 《Journal of Environmental Science and Engineering(B)》 2022年第5期155-164,共10页
The rapid increase in Water Temperature Rivers (WTR) observed globally in recent decades and projections for the coming decades under climate change scenarios make water temperature prediction essential to assess chan... The rapid increase in Water Temperature Rivers (WTR) observed globally in recent decades and projections for the coming decades under climate change scenarios make water temperature prediction essential to assess changes in aquatic biota. Statistical models for stream temperature prediction have been widely used because they are computationally simple, involve few parameters, and because of their relatively good accuracy. However, these models have not been evaluated in Peruvian Andean rivers. This work evaluates the main water temperature statistical models from the literature and fits them with data recorded in the Ichu River experimental watershed, Huancavelica-Peru. Three well-known models were reviewed: the Stefan & Preud’homme linear regression model and the Mohseni & Stefan 3- and 4-parameter logistic regression models. Ichu river water temperatures were simulated using the SWAT (Soil and Water Assessment Tool) hydrometeorological model, which defaults to the Stefan & Preud’homme model. Modifications and adjustment of coefficients of the evaluated models were configured in the SWAT code using the “Latin Hypercube Sampling” technique. The evaluated models showed poor performance in predicting the water temperature in the Ichu River with NSE (Nash-Sutcliffe Efficiency) values ranging from -2.6 to 0.49, while the modified models showed NSE values of 0.72 in all three cases. Findings suggest that the statistical models shown in the literature should be validated for Andean rivers. 展开更多
关键词 Water temperature modeling ichu River Peruvian Andes River statistical modeling
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台南盆地的地震构造 被引量:2
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作者 林明圣 萧谦丽 《地震学报》 CSCD 北大核心 2004年第4期404-409,共6页
由于发生 190 6 ,194 1,194 6 ,1994和 1999年的破坏性地震 ,对台南盆地的地震构造有了更全面的了解 ,并对台湾西南部的活动右旋走滑的义竹断裂有了新的看法 .曾熟知的梅山断裂和新化断裂不是独立的地震断裂 ,它们均属于义竹断裂的分段 ... 由于发生 190 6 ,194 1,194 6 ,1994和 1999年的破坏性地震 ,对台南盆地的地震构造有了更全面的了解 ,并对台湾西南部的活动右旋走滑的义竹断裂有了新的看法 .曾熟知的梅山断裂和新化断裂不是独立的地震断裂 ,它们均属于义竹断裂的分段 .1994年 9月 16日 ,震中在台湾海峡、台南盆地边缘的地震 ,断层面接近东西向 .此地震为台南盆地沉降历史过程中 ,右旋走滑断裂的活动剪裂所导致 .从 194 1年和 1999年地震的主震和微震记录中发现 ,这些菱形分布的地震图像 ,象征走滑断裂双轨构造中的压缩区 .基于上述研究及其它资料表明义竹断裂是台湾西南部重要的构造活动带 。 展开更多
关键词 台南盆地 地震构造 嘉南平原 台湾海峡 义竹断裂 走滑断裂
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