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Characterizing Urban Heat Islands of Global Settlements Using MODIS and Nighttime Lights Products

机译:使用MODIS和夜间照明产品表征全球定居点的城市热岛

摘要

Impervious surface area (ISA) from the National Geophysical Data Center (NGDC) and land surface temperature (LST) from MODIS averaged over three annual cycles (2003-2005) are used in a spatial analysis to assess the urban heat island (UHI) signature on LST amplitude and its relationship to development intensity, size, and ecological setting for more than 3000 urban settlements over the globe. Development intensity zones based on fractional ISA are defined for each urban area emanating outward from the urban core to the nearby non-urban rural areas and used to stratify sampling for LST. Sampling is further constrained by biome type and elevation data to insure objective inter-comparisons between zones and between cities in different biomes. We find that the ecological context and settlement size significantly influence the amplitude of summer daytime UHI. Globally, an average of 3.8 C UHI is found in cities built in biomes dominated by forests; 1.9 C UHI in cities embedded in grass/shrub biomes, and only a weak UHI or sometimes an Urban Heat Sink (UHS) in cities in and and semi-arid biomes. Overall, the amplitude of the UHI is negatively correlated (R = -0.66) to the difference in vegetation density between urban and rural zones represented by MODIS Normalized Difference Vegetation Index (NDVI). Globally averaged, the daytime UHI amplitude for all settlement is 2.6 C in summer and 1.4 C in winter. Globally, the average summer daytime UHI is 4.7 C for settlements larger than 500 square kilometers, compared to 2.5 C for settlements smaller than 50 square kilometers and larger than 10 square kilometers. The stratification of cities by size indicates that the aggregated amount of ISA is the primary driver of UHI amplitude with variations between ecological contexts and latitudinal zones. More than 60% of the total LST variances is explained by ISA for urban settlements within forests at mid-to-high latitudes. This percentage will increase to more than 80% when only USA settlements are examined.
机译:国家空间物理数据中心(NGDC)的不透水表面积(ISA)和MODIS的地表温度(LST)来自三个年度周期(2003-2005)的平均值,用于空间分析,以评估城市热岛(UHI)的特征LST振幅及其与全球3000多个城市居民区的发展强度,规模和生态环境的关系。对于从城市核心向外延伸到附近的非城市农村地区的每个城市区域,都定义了基于分数ISA的发展强度区域,并用于对LST进行分层抽样。采样受到生物群落类型和海拔数据的进一步限制,以确保不同生物群落的区域之间和城市之间的客观比对。我们发现,生态环境和居民点规模显着影响夏季白天超高强度的幅度。在全球范围内,在以森林为主的生物群落中建立的城市平均发现3.8 C UHI。 1.9 C UHI在植于草/灌木生物群落中的城市中,而在半干旱生物群落中的城市中只有弱UHI或有时是城市散热器(UHS)。总体而言,UHI的振幅与以MODIS归一化植被指数(NDVI)表示的城乡之间植被密度的差异呈负相关(R = -0.66)。从全球平均来看,所有沉降的日间UHI振幅在夏季为2.6 C,在冬季为1.4C。在全球范围内,大于500平方公里的居民点的夏季平均白天UHI为4.7 C,而小于50平方公里且大于10平方公里的居民点为2.5C。按规模划分的城市分层表明,ISA的总量是UHI振幅的主要驱动力,其生态环境和纬度区域之间存在差异。 ISA解释了中高纬度森林中城市居民点的总LST变化的60%以上。仅检查美国定居点时,该百​​分比将增加到80%以上。

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