Height Determination of Qomolangma Feng (MT. Everest) in 2005

@article{Junyong2010HeightDO,
  title={Height Determination of Qomolangma Feng (MT. Everest) in 2005},
  author={Chen Jun-yong and Zhang Yanping and Yuan Janli and Guo Chunxi and Zhang Peng},
  journal={Survey Review},
  year={2010},
  volume={42},
  pages={122 - 131}
}
Abstract Since the 1960s China has carried out several geodetic campaigns for measuring the height of Qomolangma Feng-Mt. Everest independently or in cooperation with foreign countries. Large scale geodetic field work and data processing have been done in the campaigns, dealing with positioning, height determination, gravimetry, astronomical measurement and atmospheric reflection observation etc. Some survey tasks were done in order to improve the accuracy and reliability for the height… Expand
2 Citations
New Heights of the Highest Peaks of Polish Mountain Ranges
TLDR
The most important element of this work consists of the establishment of new measurements of the heights of the highest peaks of all mountain ranges in Poland, which may result in an alteration of the officially recorded heights based on this article. Expand
Peak-bagging and cartographic misrepresentations: a call to correction
ABSTRACT Tourists put their trust in maps and guidebooks and they expect information within to be accurate. Unfortunately, vital information can often be incorrect such as the accuracy of altitudeExpand

References

SHOWING 1-10 OF 88 REFERENCES
Progress in technology for the 2005 height determination of Qomolangma Feng (Mt. Everest)
In 2005 China carried out a new geodetic campaign for the height determination of Qomolangma Feng——Mt. Everest (QF in short). The technical progresses in geodesy for the 2005 campaign are presentedExpand
THE HEIGHT OF MOUNT EVEREST
Abstract Mount Everest, the world's highest peak, was discovered by geodetic survey. Before the observations and computations of the Survey of India it was unknown, lying hidden amongst the hundredsExpand
Inversion of gravity and topography data for the crust thickness of China and its adjacent region
The data of Bouguer gravity and topography are inverted to obtain the crust thickness of China. In order to reduce the effect of regional non-isostasy we corrected the reference Moho depth in theExpand
Combined adjustment project of national astronomical geodetic networks and 2000' national GPS control network∗
TLDR
A unified national geodetic network with nearly 50000 stations is established, the high accurate three-dimensional geocentric coordinates are obtained. Expand
Deduction and Estimation of Innermost Zone Effects in Altimetry Gravity Algorithm
Based on the analysis of the FFT algorithm for the inverse Vening Meinesz formula, we present a new method to compute the components of the vertical and a formula to estimate the innermost zoneExpand
Precision Analysis of SST Gravity Field Model in China
In this paper,with China as the region in test,the potential of the new satellite gravity technique,satellite-to-satellite tracking,to improve the precision of regional gravity field model isExpand
Earth's Gravity Field Derived from Grace Satellite Tracking Data
An Earth's gravity field model IGGGRACE01S has been derived from 141 days of GRACE tracking data, including K-band, accelerometer, satellite orbit data. The model resolves the geoid with an accuracyExpand
Determination of Geoid by GPS/Gravity Data
As an application and test of the GPS/Gravity boundary value problem, a local geoid located on the N area is determined, by using 702 GPS/Gravity data for calculation and 52 GPS/levelling forExpand
Ill-posed Problem in Determination of Coordinate Transformation Parameters with Small Area's Data Based on Bursa Model
The application of GPS is often needed to transform coordinates.If the transformation parameters are solved with the GPS data in a small area,the precision of transformation parameters may be veryExpand
Application of Simulated Geoid to GPS-Leveling Interpolation
According to the topography\|isostatic theory, an isostatic\|geoid can be calculated; at the same time, the model\|geoid can be derived directly from earth's gravity field model. In this paper, theExpand
...
1
2
3
4
5
...