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显示标签为“GPS”的博文。显示所有博文
显示标签为“GPS”的博文。显示所有博文

2011年1月4日星期二

itrf2008 历元2008/01/01 部分igs站坐标

DATA SET EXPRESSED IN ITRF2008 FRAME
STATION POSITIONS AND VELOCITIES AT EPOCH 2008/01/01
DOMES NB SITE NAME ID SOLN X/Vx Y/Vy Z/Vz SIGMA x/vx SIGMA y/vy SIGMA z/vz

m-m/y m-m/y m-m/y m-m/y m-m/y m-m/y
21749S002 Tanegashima Island - GUTS-SLR Station GMSD 1 -3607665.1204147868.0573223717.2000.0010.0010.001

-0.0283-0.0099-0.01950.00020.00020.0001
21749S002 Tanegashima Island - GUTS-SLR Station GMSD 2 -3607665.1114147868.0613223717.2220.0010.0010.001

-0.0283-0.0099-0.01950.00020.00020.0001
21609M001 KUNMING KUNM 1 -1281255.8245640746.0862682879.9450.0010.0010.001

-0.03260.0023-0.01530.00010.00010.0001
21609M001 KUNMING KUNM 2 -1281255.8135640746.0802682879.9280.0010.0010.001

-0.03110.0007-0.01820.00010.00020.0001
21605M002 SHANGHAI SHAO 1 -2831733.6024675665.9223275369.4090.0010.0010.001

-0.0312-0.0105-0.01020.00010.00010.0001
21605M002 SHANGHAI SHAO 2 -2831733.6034675665.9233275369.4070.0010.0010.001

-0.0312-0.0105-0.01020.00010.00010.0001
21605M002 SHANGHAI SHAO 3 -2831733.5994675665.9203275369.3990.0010.0010.001

-0.0312-0.0105-0.01020.00010.00010.0001
21605M002 SHANGHAI SHAO 4 -2831733.5954675665.9113275369.3850.0010.0010.001

-0.0312-0.0105-0.01020.00010.00010.0001
23604S002 HSINCHU TCMS 1 -2982783.0244966660.0572658809.4230.0010.0010.001

-0.0276-0.0121-0.00920.00010.00010.0001
23603S002 TAOYUAN TWTF 1 -2994428.2484951309.2312674496.8330.0010.0010.001

-0.0326-0.0093-0.01040.00010.00010.0001
23603S002 TAOYUAN TWTF 2 -2994428.2404951309.2132674496.8170.0010.0010.001

-0.0326-0.0093-0.01040.00010.00010.0001
21602M001 WUHAN-JIUFENG WUHN 1 -2267749.5095009154.2363221290.6620.0010.0020.002

-0.0320-0.0082-0.00930.00010.00030.0002
21602M001 WUHAN-JIUFENG WUHN 2 -2267749.5065009154.2333221290.6520.0010.0010.001

-0.0316-0.0076-0.01070.00010.00010.0001
21602M001 WUHAN-JIUFENG WUHN 3 -2267749.5205009154.2643221290.6720.0010.0010.001

-0.0316-0.0076-0.01070.00010.00010.0001


<< Back to computation option setting

2010年5月31日星期一

为何GPS水平精度比垂直精度高?

这个问题有些模糊,在网上搜到的结果:
***************

因为gps是卫星图像,从高处俯视确定方位。
卫星水平和垂直就相当于把地球一点划成一个二维图像(不过图像时三维的)。
水平只要通过地球经纬度确定,不考虑地球的山峦,洼地等。垂直测定距离时,有云层,
地面漫反射等因素影响实际测定距离,就是影响了精度。而水平的话,
这些因素影响是比较小的
*******************************88
因为水平方向的变化要远大于垂直方向的变化,
所以对于高空上的卫星来说,水平方向的运动更容易分辨。 
******************************************88 

2010年5月30日星期日

坐标转换程序(xyz->geo)||convertc(gamit附带实用程序)

zhao@zhao-laptop:~$ convertc

 CONVERTC: Converts coordinate types and files
 
 Runstring:
 
  convertc
       OR  
  convertc
       OR
  converc
 
  where
 
  is the name of the input file.
   Type determined by convertc; supported:
    GLOBK apr file (new GAMIT l-file), XYZ
    GLOBK velocity file (lon/lat ENU velocity
    GLOBK glist file (lon/lat)  
  X Y Z (m) or lat lon ht (deg, m)
  Xdot Ydot Zdot OR Ndot Edot Udot (m/yr)
  is the name of the output file
  is the type of output file or coords:
    LFILE GAMIT oldstyle, spherical deg/min/sec
    APR   GLOBK apr file (new GAMIT l-file), XYZ
    VEL   GLOBK velocity file (lon/lat ENU velocity
    KML   Google Earth input (lat/lon/ht)
    GEO   Geodetic coords (lat/lon/ht), full precision
  If coords input on command-line, output is to screen
 
  Examples:
   convertc emed.apr emed.kml KML
   convertc 918129.451 -4346071.255  4561977.839 GEO
   convertc  43.36 -112.567 27.2  XYZ
   convertc  43.36 247.433  27.2  LFILE
zhao@zhao-laptop:~$ convertc 388042.6123 -740382.4073 6302001.9040  geo
Invalid screen output type geo
zhao@zhao-laptop:~$ convertc 388042.6123 -740382.4073 6302001.9040  GEO
   82.49429  -62.34047   78.2
zhao@zhao-laptop:~$

GPS IIF: 在2010年5月28日发射了

May 28, 2010
Boeing announced today (May 28) that it has acquired the first on-orbit signals from the first GPS Block IIF satellite, the inaugural spacecraft in a 12-satellite block that the company is building. The signals indicate that the spacecraft bus is functioning normally and ready to begin orbital maneuvers and operational testing.
The satellite was launched May 27 on its fourth attempt aboard a Delta IV rocket at 11:00 (EDT) from Cape Canaveral Air Force Station, Florida. At 2:33 a.m. today, the satellite separated from the rocket's upper stage, and a ground station on Diego Garcia in the Indian Ocean received the first signals from the newest member of the Air Force's GPS satellite constellation, according to Boeing.
The Air Force 19th Space Operations Squadron and Boeing's Mission Operations Support Center in El Segundo, California, confirmed that the satellite is healthy.
The satellite was placed into the slot 2 position in plane B of the GPS constellation. The satellite is expected to be set healthy for navigation uses approximately 90 days after launch.
Copyright © 2010 Gibbons Media & Research LLC, all rights reserved.

2010年5月18日星期二

GPS如何工作---资料不错--NASA

http://scign.jpl.nasa.gov/learn/gps2.htm


Three distinct parts make up the Global Positioning System. The first segment of the system consists of 24 satellites, orbiting 20,000 km above the Earth in 12-hour circular orbits. This means that it takes each satellite 12 hours to make a complete circle around the Earth. In order to make sure that they can be detected from anywhere on the Earth's surface, the satellites are divided into six groups of four. Each group is assigned a different path to follow. This creates six orbital planes which completely surround the Earth.

These satellites send radio signals to Earth that contain information about the satellite. Using GPS ground-based receivers, these signals can be detected and used to determine the receivers' positions (latitude, longitude, height.) The radio signals are sent at two different L-band frequencies. L-band refers to a range of frequencies between 390 and 1550 MHz. Within each signal, a coded sequence is sent. By comparing the received sequence with the original sequence, scientists can determine how long it takes for the signal to reach the Earth from the satellite. The signal delay is useful in learning about the Ionosphere and the Troposphere, two atmospheric layers that surround Earth's surface. A third signal is also sent to the receivers from the satellite. This signal contains data about the health and position of the satellite.

The second part of the GPS system is the ground station, comprised of a receiver and antenna, as well as communication tools to transmit data to the data center. The omni-directional antenna at each site, acting much like a car radio antenna, picks up the satellite signals and transmits them to the site receiver as electric currents. The receiver then separates the signals into different channels designated for a particular satellite and frequency at a particular time. Once the signals have been isolated, the receiver can decode them and split them into individual frequencies. With this information the receiver produces a general position (latitude, longitude, and height) for the antenna. Later, the data collected by the receiver can be processed again by scientists to determine different things, including another set of position coordinates for the same antenna, this time with millimeter accuracy.

The third part of the system is the data center. The role of the data center is two fold. It both monitors and controls the global GPS stations, and it uses automated computer systems to retrieve and analyze data from the receivers at those stations. Once processed, the data , along with the original raw data, is made available to scientists around the world for use in a variety of applications. Since global GPS sites are constructed and monitored by different institutions all over the world, there are many different data center locations.

What is GPS? How does it work? GPS in earthquakes studies Using GPS to measure earthquakes

GPS Activities

Last modified on 8/13/98 by Maggi Glasscoe (scignedu@jpl.nasa.gov)

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