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Demarcation of land-water boundary of Indian coast using MSMR data of IRS-P4 satellite at 10.65 GHz

机译:10.65 GHz的IRS-P4卫星MSMR数据划分印度海岸土地水域边界

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The microwaves are a part of electromagnetic spectrum. The frequency range from 3GHz to 30GHz is designated as microwaves. The microwaves are used extensively in remote sensing because of its unique capabilities like day and night capability and all weather capability. Because of these they have stand alone applications. Microwave sensors are either active or passive type. These sensors provide the required database with the help of emission and scattering properties of terrain under study. To mark the land water boundary of Indian Coast passive sensor radiometer is used. The brightness temperature varies with the presence of water in the soil. It is different for soil and water. The brightness temperature is different for different locations based on the emissivity. The emissivity of dry soil is more and so it has a high value of brightness temperature (TB) whereas the emissivity is low for ocean surface and so it has lower values of TB. Coastal areas contain mixture of soil and water and so its microwave temperature lies between the TB values of ocean and land surface. The multi-frequency scanning microwave radiometer (MSMR) was placed onboard IRS-P4 satellite which was launched in May 1999. This radiometer operates at 6.6, 10.65, 18 and 21GHz frequencies with dual polarization. MSMR data contains information about different geophysical parameters. From this large set of database, microwave temperature (TB) values taken at 10.65GHz with dual polarization are used to identify the land water boundary for the Indian Coast. MSMR data is available for Grid-1, Grid-2 and Grid-3 which correspond to spatial resolution of 150, 75 and 50 Km respectively. In the present study, TB data for Grid-1 is used at frequency 10.65 GHz. From the MSMR data, brightness temperature values for Indian Coast are retrieved using the data retrieval program developed in ‘C’. The program output gives the day, latitude and longitude at which data is retrieved for both vertical an--d horizontal polarizations. Data has been retrieved for 28 months from June03, 1999 to September 30, 2001. TB data values obtained are used for demarcation of land-water boundary of Indian Coast. Data values are obtained along the coastline, adjacent land surface and ocean touching the coastline. The analysis of the data at 10.65GHz frequency for land and water helps in explaining the utilization of microwave temperature for marking the land-water boundary. In the present paper analysis has been done to identify the land-water boundaries of Indian peninsula for the month of June 1999, 2000, 2001 and December 1999 and 2000. It can be used to study the coast of other locations as well.
机译:微波是电磁谱的一部分。从3GHz到30GHz的频率范围被指定为微波。由于其独特的能力和夜间能力和所有天气能力,微波在遥感中广泛使用。因为这些是独立的应用程序。微波传感器是有源或被动类型。这些传感器借助在研究下的地形的排放和散射特性的帮助下提供所需的数据库。标记印度海岸被动传感器辐射计的土地水边界。亮度温度随着土壤中的水而变化。土壤和水是不同的。基于发射率的不同位置,亮度温度不同。干燥土壤的发射率越来越多,因此它具有高值亮度温度(TB),而海洋表面的发射率低,因此其具有较低的TB值。沿海地区含有土壤和水的混合物,因此其微波温度位于海洋和陆地表面的TB值之间。将多频扫描微波辐射计(MSMR)放置在1999年5月推出的船上IRS-P4卫星上。该辐射计在6.6,10.65,18和21GHz频率下,具有双极化。 MSMR数据包含有关不同地球物理参数的信息。从这种大量数据库,使用双极化10.65GHz的微波温度(TB)值用于识别印度海岸的土地水边界。 MSMR数据可用于网格-1,Grid-2和Grid-3,其分别对应于150,75和50 km的空间分辨率。在本研究中,Grid-1的TB数据用于10.65GHz。从MSMR数据,使用“C”中开发的数据检索程序检索印度海岸的亮度温度值。程序输出给出了为垂直AN-D水平偏振检索数据的日期,纬度和经度。从1999年6月3日至9月30日期,已经检索了28个月至2001年9月30日。获得的TB数据值用于印度海岸的土地水域边界。沿着海岸线,邻近的陆地和海洋触摸海岸线获得数据值。陆地和水频率为10.65GHz频率的数据分析有助于解释微波温度的利用,以标记陆地水边界。在本文中,已经进行了在1999年6月,2000年和2000年12月的2000年6月份识别印度半岛的土地水域。它可以用来研究其他地点的海岸。

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