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81.
There is an urgent need for the development of a method that can undertake rapid, effective, and
accurate monitoring and identification of fog by satellite remote sensing, since heavy fog can cause
enormous disasters to China’s national economy and people's lives and property in the urban and coastal
areas. In this paper, the correlative relationship between the reflectivity of land surface and clouds in
different time phases is found, based on the analysis of the radiative and satellite-based spectral
characteristics of fog. Through calculation and analyses of the relative variability of the reflectivity in the
images, the threshold to identify quasi-fog areas is generated automatically. Furthermore, using the
technique of quick image run-length encoding, and in combination with such practical methods as
analyzing texture and shape fractures, smoothness, and template characteristics, the automatic
identification of fog and fog-cloud separation using meteorological satellite remote sensing images are
studied, with good results in application. 相似文献
82.
北京地区一次辐射雾的数值模拟 总被引:6,自引:2,他引:4
利用非静力中尺度模式MM5V3对2006年11月20日北京地区的一次大雾天气过程进行了数值研究。模拟结果与极轨卫星监测图像以及十二通道微波辐射计观测资料的对比表明,模式对此次雾的模拟是比较成功的,尤其是在雾区的分布位置、雾的高度以及雾的维持时间等方面。针对不同的云物理方案、长波辐射项、短波辐射项以及模式的垂直分辨率进行了4组敏感性实验。结果表明,地面的长波辐射冷却促使辐射雾的形成,而短波辐射的加热是辐射雾消散的主要原因。另外,增加模式的垂直分辨率以及选取更加详细的云微物理方案可以使模式模拟的辐射雾的结果有明显的改善。 相似文献
83.
P. D. Safai S. Kewat G. Pandithurai P. S. Praveen K. Ali S. Tiwari P. S. P. Rao K. B. Budhawant S. K. Saha P. C. S. Devara 《Journal of Atmospheric Chemistry》2008,61(2):101-118
Simultaneous measurements on physical, chemical and optical properties of aerosols over a tropical semi-arid location, Agra
in north India, were undertaken during December 2004. The average concentration of total suspended particulates (TSP) increased
by about 1.4 times during intense foggy/hazy days. Concentrations of SO4
2−, NO3
−, NH4
+ and Black Carbon (BC) aerosols increased by 4, 2, 3.5 and 1.7 times, respectively during that period. Aerosols were acidic
during intense foggy/hazy days but the fog water showed alkaline nature, mainly due to the neutralizing capacity of NH4 aerosols. Trajectory analyses showed that air masses were predominantly from NW direction, which might be responsible for
transport of BC from distant and surrounding local sources. Diurnal variation of BC on all days showed a morning and an evening
peak that were related to domestic cooking and vehicular emissions, apart from boundary layer changes. OPAC (Optical properties
of aerosols and clouds) model was used to compute the optical properties of aerosols. Both OPAC-derived and observed aerosol
optical depth (AOD) values showed spectral variation with high loadings in the short wavelengths (<1 μm). AOD value at 0.5 μm
wavelength was significantly high during intense foggy/hazy days (1.22) than during clear sky or less foggy/hazy days (0.63).
OPAC-derived Single scattering albedo (SSA) was 0.84 during the observational period, indicating significant contribution
of absorbing aerosols. However, the BC mass fraction to TSP increased by only 1% during intense foggy/hazy days and thereby
did not show any impact on SSA during that period. A large increase was observed in the shortwave (SW) atmospheric (ATM) forcing
during intense foggy/hazy days (+75.8 W/m2) than that during clear sky or less foggy/hazy days (+38 W/m2), mainly due to increase in absorbing aerosols. Whereas SW forcing at surface (SUF) increased from −40 W/m2 during clear sky or less foggy/hazy days to −76 W/m2 during intense foggy/hazy days, mainly due to the scattering aerosols like SO4
2-. 相似文献
84.
Four different mountainous locations were selected in the Valencia region, East coast of the Iberian Peninsula, for fog water collection studies. Data for 2004 were obtained by means of an instrument ensemble consisting essentially of a passive cylindrical fog water collector, a raingauge, a wind direction and velocity sensor and a temperature and humidity probe. An approximate data reduction technique was also found for this specific ensemble to eliminate the simultaneous rain water component from the fog water measurements. Main results indicate that fog water collection holds significant potential in this region, and especially for southern locations. Annual rates of fog water yield can be as high as 7.0 l/m2/day in the southern locations, in contrast to 2.0 l/m2/day collected at one site in a northern location. The highest summer fog water yield was 4.6 l/m2/day, a relatively large value. Except for the summer period, fog episodes delivering sizeable water volumes are inherently coupled to rainfall. Hourly frequencies of fog collection were also examined to show a distinct daily cycle in summer, denoting orographic fog formation during this period. Lastly, winds were analysed to resolve the most suitable directions for fog collector alignment. 相似文献
85.
京津塘高速公路雾气候特征与气象条件分析 总被引:7,自引:2,他引:5
利用1954-2002年的北京、天津和塘沽3站的雾日、雾发生时间以及气象观测资料,对京津塘高速公路沿线雾的气候特征以及气象条件进行了分析.结果发现,京津塘沿线多年平均雾日在15~19天.北京、天津两站的雾日年际变化一致.但在多年雾日变化上北京雾日数略呈逐年下降趋势,而天津、塘沽则略呈上升趋势.京津塘公路沿线雾多在凌晨到日出前后生成,在日出后逐渐消失.雾持续时间随时间变化呈指数递减.地面温度、相对湿度、风速等气象要素对京津塘高速公路沿线雾的预报具有较好的指示意义.地面温度在-5~5℃范围内、风速在0~4m·s-1和相对湿度在90%~100%范围里,雾极易发生. 相似文献
86.
2004年冬季华北平原持续大雾天气的诊断分析 总被引:26,自引:8,他引:26
利用GTS1型数字式探空仪探测的资料、NCEP 1°×1°的6小时资料和常规观测资料,对2004年冬季华北平原历史上少见的持续大雾天气进行了天气动力学诊断分析。结果表明:华北平原近地面气层900hPa以下的负涡度平流、冷温度平流和弱辐合上升运动引起该层气温下降,900-500hPa的正涡度平流、暖温度平流和辐散下沉运动造成该层气温升高,在上升和下沉运动区的界面层中形成逆温层,逆温层的高度和强度影响雾的形成和状况。夜间辐射热力强迫作用和950hPa以下的微风是大雾形成的动力因子。大雾边界层中存在的水汽饱和层是在特定的环流形势下华北平原低空盛行东和东南向岸气流,将北部海面的水汽向西向北平流到冷近地面气层中的结果。 相似文献
87.
河北省中南部一次大雾天气过程分析 总被引:20,自引:2,他引:20
对2003年11月河北省中南部大雾天气进行了分析,结果表明与稳定度有关的物理量场的变化不仅是强对流等灾害性天气的预报指标,对大雾天气也有一定的指示意义:雾是在稳定的大气层结下出现的天气现象,根据大气稳定层结的状况及变化,可以判断大雾天气的有无及其生消时间。另外,前期湿度条件的积累也是影响大雾生成的主要原因。 相似文献
88.
89.
开封大雾气候特征及预报 总被引:1,自引:0,他引:1
利用1961~2000年气象资料,分析了开封市大雾天气分布规律、天气特征,并总结出大雾产生的几种天气形势,找出预报指标。 相似文献
90.
The chemical composition of fogwater has been studied in the city of Strasbourg (France) from 1990 to 1999. During these years, fogwater samples have been collected and analysed for major ions and trace metals. This paper reports on the analysis of the collected dataset. The analysis revealed a significant decrease in acidity of approximately one pH unit over the course of the study. This decrease in acidity appears to be linked to a decrease in SO2(g) and the resulting SO42−. Trace metal concentrations have also strongly decreased over the 10-year period. Pb concentrations, following the elimination of leaded gasoline, decreased by more than one order of magnitude. 相似文献