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首页> 外文期刊>Journal of Applied Meteorology and Climatology >Fine-Resolved, Near-Coastal Spatiotemporal Variation of Temperaturein Resnonse to Insolation
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Fine-Resolved, Near-Coastal Spatiotemporal Variation of Temperaturein Resnonse to Insolation

机译:响应日照的精细分辨的近海岸时空变化

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This study uses GIS-based modeling of incoming solar radiation to quantify fine-resolved spatiotemporal responses of monthly average temperature, and diurnal temperature variation, at different times and locations within a field study area located onthe eastern coast of Sweden. Near-surface temperatures are measured by a network of temperature sensors during the spring and summer of 2011 and then used as the basis for model development and testing. The modeling of finescale spatiotemporal variationconsiders topography, distance from the sea, and observed variations in atmospheric conditions, accounting for site latitude, elevation, surface orientation, daily and seasonal shifts in sun angle, and effects of shadows from surrounding topography. Theauthors find a lag time between insolation and subsequent temperature response that follows an exponential decay from coastal to inland locations. They further develop a linear regression model that accounts for this lag time in quantifying fine-resolvedspatiotemporal temperature evolution. This model applies in the considered growing season for spatial distribution across the studied near-coastal landscape.
机译:这项研究使用基于GIS的入射太阳辐射建模来量化瑞典东部沿海地区实地研究区域内不同时间和地点的月平均温度和昼夜温度变化的精细分辨的时空响应。在2011年春季和夏季,通过温度传感器网络对近地表温度进行测量,然后将其用作模型开发和测试的基础。精细尺度时空变化的模型包括地形,距海的距离以及观测到的大气条件的变化,这要考虑场地纬度,海拔,表面方向,太阳角的每日和季节性变化以及周围地形阴影的影响。作者发现在日照和随后的温度响应之​​间存在一个从沿海到内陆位置呈指数衰减的滞后时间。他们进一步开发了线性回归模型,该模型在量化精细分辨的时空温度演变时考虑了该滞后时间。该模型在所考虑的生长季节中适用于所研究的近岸景观的空间分布。

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