Local Climate Zones for Urban Temperature Studies
Iain D. Stewart,Timothy R. Oke +1 more
TL;DR: The Local Climate Zone (LCZ) classification system as discussed by the authors was developed to address the inadequacies of urban-rural description, and consists of 17 zone types at the local scale (102 to 104 m).
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Abstract: The effect of urban development on local thermal climate is widely documented in scientific literature. Observations of urban–rural air temperature differences—or urban heat islands (UHIs)—have been reported for cities and regions worldwide, often with local field sites that are extremely diverse in their physical and climatological characteristics. These sites are usually described only as “urban” or “rural,” leaving much uncertainty about the actual exposure and land cover of the sites. To address the inadequacies of urban–rural description, the “local climate zone” (LCZ) classification system has been developed. The LCZ system comprises 17 zone types at the local scale (102 to 104 m). Each type is unique in its combination of surface structure, cover, and human activity. Classification of sites into appropriate LCZs requires basic metadata and surface characterization. The zone definitions provide a standard framework for reporting and comparing field sites and their temperature observations. The LCZ s...
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Citations
Land Surface Temperature Retrieval From Landsat 8 Thermal Infrared Data Over Urban Areas Considering Geometry Effect: Method and Application
Chen Ru,Si-Bo Duan,Xiaoguang Jiang,Zhao-Liang Li,Yazhen Jiang,Huazhong Ren,Pei Leng,Maofang Gao +7 more
TL;DR: A radiative transfer equation (RTE)-based single-channel method was developed to retrieve LST with urban geometry effect correction from the Landsat 8 thermal infrared (TIR) data in band 10, and the results indicate that UHII calculated from L ST withUrban heat island intensity (UHII) is lower than that calculate from LST without urban geometryEffect correction.
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TL;DR: In this paper, the authors applied the weather research and forecasting model to simulate UHI-induced circulation in the presence of background wind and found that the strong UHIC flow pattern is characterized by upstream back-currents and returned leeside inflows.
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James Richard Anderson,Ernest E. Hardy,John T. Roach,Richard E. Witmer +3 more
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The energetic basis of the urban heat island
Abstract: In such a framework the field of urban meteorology may be judged to be at an early stage and to be evolving in a rather unbalanced fashion. The literature of the past 150 years is replete with studies of ’urban effects’ carried out at levels 1 and 2. Usually they are concerned with simple description or statistical analysis based upon empirical evidence from a single city. With the exception of a very few notable studies, attention to the processes (i.e. the causes underlying the observed effects) and to physico-mathematical modelling has been restricted to the past decade. Of course it is not expected, nor indeed may it be desirable, that research in a field should progress in a simple manner through the sequence 1-4, but two important points should be evident. First. as time progresses the bulk of research in a field should move to higher levels of enquiry. Second, the predictive power of processresponse models is limited by the extent to which the processes are understood. Some special difficulties have contributed to this unsatisfactory state of the field including : (1) the inherent complexity of the city-atmosphere system. The atmospheric state is a response to exchanges of energy, mass and momentum covering a wide range of space and time scales; in urban areas the sources and sinks for these exchanges are located in an extremely heterogeneous fashion and involve significant anthropogenic as well as natural factors; (2) the lack of clear conceptual/theoretical frameworks for enquiry especially in the light of the complications placed upon conventional theory by (1) ; (3) the expense and difficulty of observation in cities. Commonly one must deal with conditions within a relatively large volume of air (typically lo2 to lo3 km3) containing significant spatial and temporal variability thereby creating sampling problems. Moreover there are restrictions on the use of observation systems (towers, aircraft, balloons, acoustic radar) not normally encountered in uninhabited terrain. Here we will use the example of the urban ‘heat island’ effect to illustrate the state of urban meteorological research. This will include a condensed review of our understanding
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A land use and land cover classification system for use with remote sensor data
James Richard Anderson,Ernest E. Hardy,John T. Roach,R. Witmer +3 more
TL;DR: A land use and land cover classification system for use with remote sensor data provides a standardized framework for classifying land use and land cover throughout the country.
3.7K