ITU-R REPORT RS 2095-2007 Sharing of the 36-37 GHz band by the fixed and mobile services and the Earth exploration-satellite service (passive)《共享36-37 GHz频段的固定和移动业务以及地球探测卫星业务(无源)》.pdf
《ITU-R REPORT RS 2095-2007 Sharing of the 36-37 GHz band by the fixed and mobile services and the Earth exploration-satellite service (passive)《共享36-37 GHz频段的固定和移动业务以及地球探测卫星业务(无源)》.pdf》由会员分享,可在线阅读,更多相关《ITU-R REPORT RS 2095-2007 Sharing of the 36-37 GHz band by the fixed and mobile services and the Earth exploration-satellite service (passive)《共享36-37 GHz频段的固定和移动业务以及地球探测卫星业务(无源)》.pdf(27页珍藏版)》请在麦多课文档分享上搜索。
1、 Rep. ITU-R RS.2095 1 REPORT ITU-R RS.2095 Sharing of the 36-37 GHz band by the fixed and mobile services and the Earth exploration-satellite service (passive) (2007) TABLE OF CONTENTS Page 1 Introduction 2 2 EESS (passive) . 2 2.1 Applications 2 2.2 Passive sensor parameters. 2 2.3 Interference cri
2、teria. 4 3 Fixed and mobile service parameters . 5 3.1 Fixed service (FS). 5 3.2 Mobile service (MS). 6 4 Simulation studies 7 4.1 General simulation methodology 7 4.2 Simulation study number 1. 7 4.3 Simulation study number 2. 9 4.4 Simulation study number 3. 11 4.4.1 P-P FS systems. 11 4.4.2 P-MP
3、FS systems . 15 4.5 Simulation study number 4. 17 4.6 Summary of sharing study results. 20 4.6.1 Sharing between the FS and the EESS (passive) . 20 4.6.2 Sharing between the MS and the EESS (passive) 22 5 Mitigation techniques . 22 5.1 EESS (passive) 22 5.2 FS 24 5.3 MS. 26 6 Summary and conclusions
4、 26 7 Supporting documents 27 2 Rep. ITU-R RS.2095 1 Introduction The purpose of this report is to summarize the result of the studies on sharing the 36-37 GHz band by the fixed and mobile services and the Earth exploration-satellite service (EESS) (passive) 2 EESS (passive) 2.1 Applications The ban
5、d 36-37 GHz is of primary interest to measure rain, snow, ocean ice and water vapour. This band is also called a window. This band is essential for the precise knowledge of the hydrological cycle or global water circulation. For the measurement of surface parameters, some radiometric window channels
6、 must be selected to determine the corresponding expected parameters for the ocean or land surfaces. For ocean surfaces, the main parameters that are measured over the ocean surfaces are: salinity, wind speed, liquid clouds, water vapour and sea surface temperature. Liquid clouds are obtained via me
7、asurements at 36 GHz. Five frequencies (6, 10, 18, 24 and 36 GHz) are necessary for determining the above main parameters. For land surfaces, the problem is more complex due to high temporal and spatial variability of surface characteristics (from snow/ice covered areas to deserts and tropical rain
8、forests). Over this kind of surface, the retrieved parameters are: vegetation biomass, cloud liquid water, integrated water vapour, soil moisture and surface roughness. The use of the 36 GHz allows the retrieval of the contents of the cloud liquid vapour and of the snow covered areas. It has been sh
9、own that this band is the most suitable band for snow detection and has been used for the last 20 years for climatological studies of snow, sea ice, soil moisture, microwave vegetation index and land surface temperature. Measurements at 36 GHz have shown the capability to derive the snow water equiv
10、alent. The use of spaceborne remote sensing techniques offers a way to complement and extend conventional ground based measurements of snow to regional and global scales. There is a continuing need to determine the snow water equivalent and its variability over large areas for climatological and hyd
11、rological applications. In addition to the snow water equivalent, it is also possible to derive from spaceborne microwave remote sensing measurements, the snow depth based on the physics of the microwave radiation. The 36-37 GHz band measurements also provide auxiliary parameters for other remote se
12、nsing instruments. Spaceborne radar altimeters are currently operated on a global basis above ocean and land surfaces, with important applications in oceanography and climatology. In order to remove refraction effects due to the atmosphere, the utilization of highly accurate altimetric data require
13、that they are complemented with a set of auxiliary passive measurements around 18.7, 23.8 and 36.5 GHz. In that case, the goal of the 36 GHz band measurements is to compute the tropospheric delay in order to enhance the accuracy of the data retrieved through the altimeters. It is to be noted that al
14、l the above usages are fully operational. 2.2 Passive sensor parameters Table 1 summarizes the parameters of conical scanning passive sensors that are or will be operating in the 36-37 GHz band as illustrated in Fig. 1. Rep. ITU-R RS.2095 3 TABLE 1 Passive sensor parameters Type of sensor MADRAS AMS
15、R-E CMIS Channel bandwidth (GHz) 1 1 1 Pixel size across track (diameter of the pixel) (km) 38 7.8 12 Incidence angle i at footprint centre (degrees) 52.3 55 55.7 Offset angle to the nadir or half cone angle (degrees) 44.5 47.5 47 Polarization H H,V H,V Altitude of the satellite (km) 817 705 833 Max
16、imum antenna gain (dBi) 45 53 55 Reflector diameter (m) 0.65 1.6 2.2 Half power antenna beamwidth 3dB(degrees) 1.8 0.4 0.52 Useful swath (km) 1 607 1 450 1 782 Antenna pattern Fig. 2 Fig. 3 N/A FIGURE 1 Geometry of conical scan passive microwave radiometers 4 Rep. ITU-R RS.2095 The antennas of passi
17、ve sensors are modelled according to the following figures. FIGURE 2 MADRAS antenna gain pattern at 36 GHz FIGURE 3 AMSR-E antenna gain pattern at 36 GHz 2.3 Interference criteria Recommendation ITU-R RS.1029 Interference criteria for satellite passive remote sensing recommends permissible interfere
18、nce levels and reference bandwidths for use in any interference assessment or sharing studies. The permissible interference levels for the 36-37 GHz band are 156 dBW in a reference bandwidth of 100 MHz for current passive sensors, and 166 dBW in a reference bandwidth of 100 MHz for future passive se
19、nsors that are more sensitive than the currently operational passive sensors. The first number is indicated for sharing conditions circa 2003; while the second number is for scientific requirements that are technically achievable by sensors in the next 5-10 years. Recommendation ITU-R RS.1029 also s
20、pecifies that these interference levels should not be exceeded for more than 0.1% of sensor viewing area, described as a measurement area of a square on the Earth of 10 000 000 km2unless otherwise justified. Rep. ITU-R RS.2095 5 3 Fixed and mobile service parameters 3.1 Fixed service (FS) FS systems
21、 in this band can generally be characterized as either point-to-point (P-P) or point-to-multipoint (P-MP) systems. Table 2 summarizes the parameters of P-P system that could operate in the 36-37 GHz that were considered in these studies. TABLE 2 P-P FS station parameters Parameter FS-1 FS-2 Modulati
22、on type O QPSK Distance between stations (one hop length) (km) Around 2 From 0.5 to 20 Point-to-point Channel capacity (Mbit/s) 2.048; 8.448; 34.368 Receiver sensitivity (BER up to 106) (dBW) Up to 117 Transmitter power (dBW) 18.24 dBW/30 MHz (= 15 mW/30 MHz) 13 to 7 Antenna gain (dBi) 37 39-42 Ante
23、nna diameter (m) 0.4-0.5 Antenna type Parabolic Antenna pattern Rec. ITU-R F.1245 Max. feeder loss (dB) 0.5 Frequency grid Rec. ITU-R F.749 Table 3 summarizes the parameters of one possible type of terrestrial P-MP station that could operate in the 36-37 GHz. TABLE 3 P-MP FS station parameters Param
24、eter Central (hub) station Customer terminal station Modulation QPSK Access method Time division multiplex (TDM) Bandwidth/carrier (MHz) 28 28 Antenna type Sectoral antenna Dish Antenna gain (dBi) 17 39 Antenna beamwidth (degrees) 45 1.4 Number of active carriers/sector 4 4 Number of sectors 8 6 Rep
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