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Modeling the combined impact of climate change and sea-level rise on general circulation and residence time in a semi-enclosed sea

机译:建模气候变化和海平面上升对半封闭海洋综合循环和停留时间的综合影响

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This study provides an assessment of possible changes in the general circulation and residence time in the Persian Gulf under potential future sea-level rise and changes in the wind field due to the climate change. To determine the climate-change-induced impacts, Mike 3 Flow Model FM was used to simulate hydrodynamic and transport processes in the Persian Gulf in both historical (1998-2014) and future periods (2081-2100). Historical simulation was driven by ERA-Interim data. A statistical approach was employed to modify the values and directions of the future wind field obtained from the Representative Concentration Pathway 4.5 and 8.5 (RCP4.5 and RCP8.5, respectively) scenarios derived from CMCC-CM model of the fifth phase of the Coupled Model Intercomparison Project (CMIP5). The numerical model was calibrated and validated using measured data. Results indicated that in the historical period, residence time ranged between values of less than a month in the Strait of Hormuz and 10 years in the semi-enclosed area close to the south of Bahrain. The changes in wind field based on RCP 8.5 scenario were found to be the most disadvantageous for the Persian Gulfs capacity to flush dissolved pollutants out. Under this scenario, residence time would be 17% longer than that of historical one. This is mainly because the change in the wind field is large enough to overwhelm general circulation, showing a relationship between the residence time and the residual circulation. Impact of change in the wind field according to RCP 4.5 scenario on the modeled residence time is negligible. The numerical outputs also showed that the sea-level rise would slightly decrease the current velocity, resulting in a negligible increase in residence time. The findings of this study are intended to support establishing climate-adaptation management plans for coastal zones of the studied area in line with sustainable development goals.
机译:本研究规定了对波斯湾的普通循环和住宅时间可能变化的评估,在波斯湾的潜在未来的海平面上升和由于气候变化导致风领域的变化。为了确定气候变化诱导的影响,Mike 3流量模型FM用于模拟波斯湾的流体动力和运输过程,历史(1998-2014)和未来时期(2081-2100)。历史模拟由ERA-INSIMIM数据驱动。采用统计方法来修改从代表浓度途径4.5和8.5(RCP4.5和RCP8.5)获得的未来风场的值和方向,其中源自耦合的第五阶段的CMCC-CM模型的情况型号互通项目(CMIP5)。使用测量数据校准和验证数值模型。结果表明,在历史时期,住宿时间在Hormuz海峡两岸的价值不到一个月之间,在巴林南部的半封闭区域中10年。基于RCP 8.5情景的风场变化被发现是波斯湾普拉斯溶解污染物的最不利的污染物。在这种情况下,停留时间比历史人员长17%。这主要是因为风场的变化足够大,以压倒一般循环,显示停留时间与残余循环之间的关系。根据RCP 4.5场景在模型停留时间的情况下,风场变化的影响可忽略不计。数值输出还表明,海平面上升将略微降低当前速度,从而可以忽略不计的停留时间。本研究的调查结果旨在支持符合可持续发展目标的研究区沿海地区的气候适应管理计划。

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