武汉市热岛强度分区与规划应对策略

城市热岛强度分区是城市通风环境改善的前期准备工作。通过空间信息技术方法,提取不同土地类型,并结合建成区热岛强度指数划分武汉市热岛及冷空气生成区。结果表明:用地类型与地表温度存在明显的相关性,大部分水域处于低温区及次低温区,高温区不存在林草地和耕地,城市建设用地主要分布在高温区内;热岛区域大部分分布在武汉市主城区范围内,冷空气生成区位于城市热岛的周边,主城区范围内的大型湖泊、河流和公园绿地对热岛进行分隔。由此提出,对武汉市各个气候功能片区采取分类规划改善策略。     

基于卫星遥感的京津冀热环境效应分析

为探究北京城区和京津冀城市群等不同尺度上地表热环境时空格局变化以及与大气污染和污染排放的关系,利用Landsat-58、Terra MODIS和Aura卫星上OMI等多期数据,采用普适性单窗算法反演了不同区域的地表温度强度,并结合京津冀重点行业NOX排放量和区域NO2柱浓度空间分布数据,分析了2001—2016年北京及京津冀地区大气污染、能源消耗和城市热力格局之间的关系。结果表明:北京市热岛分布具有显著的地域性,高地表温度与相对较低地表温度集聚与相间分布并存,建成区城市热岛效应明显; 2001—2016年随着城市的快速发展,城区快速向外蔓延,北京城市的热场强度逐年加强,范围逐年向东、向南扩大;热岛高强度范围与NO2高污染区、NOX高排放区有较好的一致性,热岛强度的分布特征有助于大气污染物"热量"网络的规划,卫星热红外遥感可提供必要的技术支撑。     

京津冀秋冬季工业生产热异常遥感监测探讨

为全面、客观掌握工业生产热排放对大气污染的影响,利用遥感手段分析了2018—2019年秋冬季京津冀工业生产热排放及其同比变化。结果显示:2018—2019年秋冬季,京津冀地区工业热异常点数量及秋冬热异常点辐射功率(FRP秋冬)较上年同期明显增加,工业生产活动规模及强度同比有所扩大,区域PM2. 5浓度呈增长趋势。根据FRP秋冬分布特点可将京津冀工业生产分为3类,密集型、分散型和稀少型。工业生产密集型城市FRP秋冬通常 1 500 MW,较为典型的城市如唐山、邯郸,FRP秋冬可达2 000 MW以上甚至上万MW,这些城市的空气质量也相对较差;保定是工业生产分散型城市,该城市热异常点增长显著,FRP秋冬也可达2 000 MW以上,但空间分布分散;工业生产稀少型城市热异常点较少且空气质量相对较好。     

基于TM资料对上海区域热环境特征的分析

为了揭示城市热岛(UHI)形成机制,以TM卫星遥感资料为主要数据源,结合地面自动气象站(AWS)实测的气象资料,利用地表能量平衡参数化(SEBAL)的方法估算了净辐射通量和土壤热通量,分析了上海区域热环境特征.结果表明,TM地表温度与AWS实测地表温度具有较好的一致性;不同类型地表其地表温度差异明显,城市道路是城市中重要热量来源,绿地和水体面积的增加能有效地减轻城市热岛强度,同时也表明了卫星遥感资料在城市气候环境研究中的潜在价值.     

基于遥感的海域环境变化监测分析

以杭州湾海域和连云港周边海域为研究对象,基于Landsat-5、Landsat-9的多光谱和热红外数据,对研究区的海域岸线和温度场信息进行提取,分析海域岸线变迁和温度分布变化特征。结果显示,研究区的海域岸线变化均较显著;海域温度在核电站运行前较为均匀,无明显温度分异,核电站运行后,因温排水排放,核电站周边海域温度出现明显分异;Landsat-9热红外数据温度反演结果可靠,可用于监测温排水对海域环境的影响。     

利用TM影像监测和评价大亚湾温排水热污染

水热污染一直是环保工作中一个关注焦点,在对水热污染的日常环境监测中,往往存在测量不方便、区域评估不准等问题。如何充分利用遥感技术便捷、大范围、动态等特点对水热污染进行有效地监测和环境评价是本研究的重点。文章利用多个时相的TM数据热红外波段影像,对广州大亚湾核电站温排水水域进行了水温的反演,有效地对核电站温排水强度、扩散范围和环境影响进行了评价。研究证明,遥感技术能够有效地完成水热污染的监测和环境影响评估。     

利用植被供水指数法监测干旱的研究

利用FY-1D/AVHRR数据通道1、2的反射率计算植被指数和通道4、5的亮温计算作物冠层温度,进而求出植被供水指数可监测干旱状况.本文简单介绍了利用FY-1D/AVHRR数据植被供水指数法监测生长季的干旱状况.研究表明,该方法所得结果从总体趋势看,与实际情况基本吻合.因此,植被供水指数法适用于生长季大范围的干旱监测.     

基于多时相卫星数据的采砂场遥感调查研究——以青海省湟水流域为例

文章采用多源多时相高分辨率遥感影像作为数据源,以ArcGIS、Erdas、Envi等遥感地信软件为信息提取平台,对青海省湟水流域的采砂场进行遥感调查分析。结果显示：①采砂场主要分布在湟水流域城市周边,其中,在用采砂场分布较密集,如西宁、湟中、平安附近分布较集中,而停用采砂场分布相对比较均匀;②采砂场共305处,其中长期和临时采砂场占重要比例,达73%,经过平整或绿化的停用采砂场较少,而停用且无整改及整改中的采砂场数量仍较多,是已整改的2倍;③长期采砂场面积规模占所有类型总面积的比重最大,达三分之二,而经过平整或已绿化的规模仅0.75 km²。研究以期对环境监察管理提供技术支撑,为后续的研究和砂场的高效精准管理提供技术方法和科学依据。     

武汉市秋季PM2.5中硫酸盐、硝酸盐理化特征及影响因素

为了解武汉市秋季PM_(2.5)中硫酸盐、硝酸盐理化特征,2016年9—11月利用热还原法在线连续监测分析系统对此进行了采样分析,并同步收集气象因子和离子色谱方法监测结果。结果表明,硫酸盐、硝酸盐的热还原分析方法与离子色谱法的相关系数分别为0.88、0.94;PM_(2.5)中硫酸盐、硝酸盐的水溶性部分占比达92.5%,难溶性部分为7.5%;空气质量为优、良和轻度污染时,硫酸盐、硝酸盐与PM_(2.5)的占比分别为45%、42%、45%;硫酸盐、硝酸盐在降水日和非降水日平均质量浓度分别为(19.6±18.5)μg/m~3和(31.0±9.1)μg/m~3;硝酸盐与硫酸盐的质量比为1.1,高于国内其他城市,与武汉市机动车保有量大幅增加有关。     

西藏拉萨市热岛效应及其影响因子分析

采用2001年、2004年以及2007年三年的EOS/MODIS遥感信息反演的地面温度以及多年常规气象观测资料,讨论了拉萨市热岛现象及其可能影响因子。结果表明:(1)热岛强度的年、季节变化呈现逐渐增强的趋势,其中,冬季的热岛强度最强,其次是春季,秋季和夏季的热岛效应较弱;高温区基本位于城市中心或者县城所在地及其周围,低温区主要集中在各县的郊区;近年来拉萨地区的城市高温区域逐渐扩大,有些高温中心可能向某些区域偏移;遥感资料所获取的地表温度与平均气温之间存在一定的正相关性。(2)无论是年变化,还是季节变化,热岛强度都与风速呈正相关,与日照时数呈负相关,与蒸发量的相关在夏季和冬季分别呈正相关、负相关的相反状况;地表温度与植被分布具有较好的负相关关系,即在城区存在较高的地表温度分布和较小的NDVI,过渡到郊区具有温度减小、NDVI增加的特征;随着城市化进程的加剧,建筑面积不断扩大,人类活动明显增加,排放至大气的人为热增加,这些因素都可能导致热岛强度的增强。     

Evaluating the urban climate of a typically tropical city of northeastern Brazil

This study attempted to assess a bioclimate index and the occurrence of an urban heat island in the city of Campina Grande, northeastern Brazil, using data taken from mobile measurements and Automatic Weather Stations (AWS). The climate data were obtained during two representative months, one for the dry season (November 2005) and one for the rainy season (June 2006) at seven points in an urban area. Ten-minute air temperatures recorded by an AWS installed in urban areas were compared to those from a similar station located in a suburban area to assess the urban heat island (UHI). The data were collected using a 23X data logger (Campbell Scientific, Inc.) programmed for collecting data every second. The thermal discomfort level was analyzed by Thom’s discomfort index (DI), and an analysis of variance was applied for assessing if there was any statistically significant difference at the 1% and 5% significance level of thermal comfort among points. Mann–Kendall statistical test was used for identifying possibly significant trends in a time series for air temperature, relative humidity, and class A pan evaporation for the city of Campina Grande. The present study found UHI intensities of 1.48°C and ??0.7°C for the months taken as representative of the dry and rainy seasons, respectively. Summer in the city has partially comfortable conditions while the winter is fully comfortable. There are significant changes in DI hourly values between seasons. Only during the rainy season did all points of the city have a comfortable condition until 8:19 h, at which time they become partially comfortable for the rest of the day. Results indicated that there was a 1.5°C increase in air temperature and a 7.2% reduction in relative humidity throughout the analyzed time series. The DI also showed a statistically significant increasing trend (Mann–Kendall test, p?<?0.01) for the dry and rainy seasons and annual period of approximately 1°C in the last 41 years in the city of Campina Grande.     

An approach to analyzing the intensity of the daytime surface urban heat island effect at a local scale

A landscape index LI is proposed to evaluate the intensity of the daytime surface urban heat island (SUHI) effect at a local scale. Three aspects of this landscape index are crucial: the source landscape, the sink landscape, and the contribution of source and sink landscapes to the intensity of the SUHI. Source and sink landscape types are identified using the thermo-band of Landsat 7 with a spatial resolution of 60 m, along with appropriate threshold values for the Normalized Difference Vegetation Index, Modified Normalized Difference Water Index, and Normalized Difference Built-up Index. The landscape index was defined as the ratio of the contributions of the source and sink landscapes to the intensity of the SUHI. The intensity of the daytime SUHI is assessed with the help of the landscape index. Our analysis indicates the landscape index can be used to evaluate and compare the intensity of the daytime SUHI for different areas.     

Quantifying urban heat island intensity in Hong Kong SAR, China

This paper addresses the methodological concerns in quantifying urban heat island (UHI) intensity in Hong Kong SAR, China. Although the urban heat island in Hong Kong has been widely investigated, there is no consensus on the most appropriate fixed point meteorological sites to be used to calculate heat island intensity. This study utilized the Local Climate Zones landscape classification system to classify 17 weather stations from the Hong Kong Observatory’s extensive fixed point meteorological observation network. According to the classification results, the meteorological site located at the Hong Kong Observatory Headquarters is the representative urban weather station in Hong Kong, whereas sites located at Tsak Yue Wu and Ta Kwu Ling are appropriate rural or nonurbanized counterparts. These choices were validated and supported quantitatively through comparison of long-term annual and diurnal UHI intensities with rural stations used in previous studies. Results indicate that the rural stations used in previous studies are not representative, and thus, the past UHI intensities calculated for Hong Kong may have been underestimated.     

城市化进程对城市热岛效应因子的对比分析

采用1990～2004年乌鲁木齐市和其郊区的温度差值作为衡量其城市热岛效应的标准,以乌鲁木齐市城市化七项指标作为城市热岛效应的形成因子.通过多元回归模型分析了各热岛效应因子对城市热岛的影响.文章主要结论包括乌鲁木齐市各热岛效应因子时城市热岛的影响是不同的,居民生活条件的改善和公共基础设施的改善减轻了热岛效应的影响,热岛效应也符合环境库兹涅茨曲线规律.     

Monitoring the effect of urban green areas on the heat island in Athens

The role of urban green areas in the microclimatic conditions of cities, during summer, is investigated in this paper through monitoring campaigns carried out at the National garden, at the city centre of Athens. Two types of investigations were carried out: i) a microscopic one that investigated the thermal conditions inside the Garden and the immediate surrounding urban area and ii) a macroscopic one that compared the temperature profile of the Garden with that of the greater city centre area. It was concluded that in microscopic level, the temperature profile inside the National Garden and the immediate surrounding urban area did not showed a clear evidence of the influence of the Garden and it was dependent on the characteristics of each location. In a macroscopic scale, the Garden was found cooler than the other monitored urban locations and temperature differences were mainly greater during the night, especially in streets with high building height to street width (H/W) ratio and low traffic, while in streets with high anthropogenic heat during the day, the biggest temperature differences were recorded during the day.     

Temporal and spatial characteristics of the urban heat island during rapid urbanization in Shanghai, China

Based on meteorological data from 1978 to 2007, we investigated the annual, seasonal, and fixed hourly variations of Shanghai urban heat island (UHI) in urban and suburban areas and spatial distribution of UHI. The results demonstrated a remarkable interannual increase of UHI intensity in Shanghai. The UHI was the strongest in autumn and the weakest in summer, as a consequence of the prevailing weather conditions. Similar to previous studies of other cities, the UHI in Shanghai was stronger in the nighttime than in the daytime. The SW–NE cross section followed the general cross section of the typical UHI described by Oke (1987) who defines its characteristic parts as “cliff”, “plateau”, and “peak”. Analysis of the association of UHI and urbanization indicated that the UHI increased with the expansion of population and rapid increase of gross domestic product. The continuous increase of power consumption and area of paved road and decrease of area of cropland caused the growth of UHI intensity. Green land had a positive effect on mitigation of heat island based on an inversed U-shaped curve with UHI intensity.     

Simulation of mixing depths incorporating the urban heat island effect

The main objective of this paper was to establish the effect of anthropogenic heat flux on the formation of mixing depth specially in urban areas. In this study an energy balance mixing depth model was developed for the simulation of mixing depth incorporating the heat island effect. To demonstrate the effect of heat island, mixing depths were simulated under two conditions. Under the first condition, hourly gridded anthropogenic heat flux and variant surface characteristics were considered, while under the second condition anthropogenic heat flux term was ignored and constant surface characteristics were considered throughout the modelling domain. The release of anthropogenic heat flux in the urban environment was found to be responsible for the growth of the unstable layer in the lower atmosphere even during the night. This resulted in higher mixing depth values in urban areas compared to the surrounding countryside. The maximum differential surfaces sensible heat flux between urban and rural areas was estimated as 130 W/m². From the simulation of mixing depth, it was revealed that the maximum increment in mixing depth in urban areas was 300 m due to the heat island effect. This increment in mixing depth in urban areas can provide an extra space for dilution and mixing of pollutants.     

佳木斯大气污染物扩散影响因素及区域探究

对影响佳木斯市大气污染物扩散的因素进行了分析。结果表明,大气稳定度、垂直和水平温度梯度、低空风场引起的平流动力输送、地面粗糙度、湍流运动、雨雾等都不同程度地影响大气污染物的扩散,以一定的传输和扩散规律决定城市大气污染水平的高低,并由此使局部区域污染程度各不相同。城市热岛效应和温度层结是影响大气污染物扩散的重要因素。影响区域主要为城市主导风向下风向的城市东部地区。