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首页> 外文期刊>ournal of the Meteorological Society of Japan >Urban Climate Projection by the WRF Model at 3-km Horizontal Grid Increment: Dynamical Downscaling and Predicting Heat Stress in the 2070’s August for Tokyo, Osaka, and Nagoya Metropolises
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Urban Climate Projection by the WRF Model at 3-km Horizontal Grid Increment: Dynamical Downscaling and Predicting Heat Stress in the 2070’s August for Tokyo, Osaka, and Nagoya Metropolises

机译:WRF模型在3 km水平网格增量上对城市气候的预测:动态缩小尺度并预测2070年8月东京,大阪和名古屋都会的热应力

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摘要

This study presents the projected urban climate for the 2070s’ August in the three largest urban areas, Tokyo, Osaka, and Nagoya in Japan. To accurately evaluate the urban climate, the simulations use the Weather Research and Forecast (WRF) model with 3-km grid increment coupled to an urban canopy model (UCM). To project future urban climate, the simulations apply dynamical downscaling to three GCMs (MIROC3.2-medres, MRI-CGCM2.3.2a, CSIRO-Mk3.0) and use the ensemble average for results. The results provide estimates of the heat stress to future residents of Tokyo, Osaka, and Nagoya.The WRF-UCM model reproduces the observed spatial distribution of the surface air temperature in the 2000s’ August, giving an all-domain mean bias of -1.2°C and RSME of 2.7°C. For Tokyo, Nagoya, and Osaka, these biases are -0.6, -0.1, and -0.4°C. Moreover, the diurnal temperature variations at these urban stations are well reproduced. The projected monthly average August temperatures in the 2070s are about 2.3°C higher than those in the 2000s at the three urban areas and comparable to those in the record-breaking hot summer of 2010. (Predictions by individual ensemble members differ by 0.8-1.2°C.) As a result, urban areas will experience uncomfortable sleeping nights nearly every day in August, with roughly as many heat-induced sleeping-discomfort nights as those in 2010. Moreover, application of the wet-bulb globe temperature (WBGT) shows that people in Tokyo will be warned not to strenuously exercise outdoors for 62% of the daytime hours in the 2070s, a sharp increase from the 30% of the 2000s. (Predictions by individual ensemble members range from 54-67%). Osaka and Nagoya will have even more restrictions on outdoor exercise. Finally, the urban heat island intensity is 1.5°C in Tokyo of the 2070s, comparable to the background climate warming of 2.3°C.
机译:这项研究提出了日本东京,大阪和名古屋这三个最大的城市地区2070年代8月的预计城市气候。为了准确评估城市气候,模拟使用天气研究和预报(WRF)模型,并以3公里的网格增量与城市雨棚模型(UCM)耦合。为了预测未来的城市气候,模拟对三个GCM(MIROC3.2-medres,MRI-CGCM2.3.2a,CSIRO-Mk3.0)应用了动态降尺度,并使用集合平均值作为结果。结果提供了对东京,大阪和名古屋未来居民的热应力的估计.WRF-UCM模型再现了2000年代8月观测到的地面气温的空间分布,全域平均偏差为-1.2 °C和RSME为2.7°C。对于东京,名古屋和大阪,这些偏差是-0.6,-0.1和-0.4°C。此外,这些城市站的昼夜温度变化得到了很好的再现。预计三个城市地区2070年代的8月月平均温度比2000年代的8月平均温度高约2.3°C,与2010年破纪录的炎热夏天的温度相当。(单个乐团成员的预测相差0.8-1.2因此,城市地区几乎在八月份的每一天都会经历令人不舒服的睡眠之夜,与热量引起的睡眠不适之夜的数量大约是2010年的水平。此外,湿球温度(WBGT)的应用研究表明,到2070年代,东京的人们将被警告不要在白天进行62%的白天剧烈运动,比2000年代的30%急剧增加。 (单个合奏成员的预测范围为54-67%)。大阪和名古屋将对户外运动施加更多限制。最后,2070年代东京的城市热岛强度为1.5°C,与背景气候变暖2.3°C相当。

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