Summer warming in the East Antarctic interior triggered by southern Indian Ocean warming. [PDF]
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Origin and evolution of the North Atlantic Oscillation. [PDF]
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Geoidal Geopotential and World Height System
Studia Geophysica et Geodaetica, 1999The geoidal geopotential value of W 0 = 62 636 856.0 ± 0.5m 2 s −2 , determined from the 1993 –1998 TOPEX/POSEIDON altimeter data, can be used to practically define and realize the World Height System.
Milan Burša +7 more
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Autocorrelation of Northern Hemisphere Geopotential Heights
Monthly Weather Review, 1983Abstract Local autocorrelation statistics for the Northern Hemisphere geopotential height field are presented for different seasons and tropospheric pressure levels. Values are generally much higher than those calculated from time series of outgoing infrared radiation or eddy heat fluxes. The largest one-day lag autocorrelation values are observed over
D. S. Gutzler, K. C. Mo
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Deriving orthometric height using global geopotential models (GGMs)
2016 7th IEEE Control and System Graduate Research Colloquium (ICSGRC), 2016The purpose of this paper is to evaluate the orthometric height derived by combination of Global Navigation Satellite System (GNSS) data and global geoid height information over Peninsular Malaysia. The global geoid height information is derived from recent Global Geopotential Models (GGMs); combined and satellite-only solution.
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Monitoring the Madden–Julian oscillation with geopotential height
Climate Dynamics, 2016This paper examines the three-dimensional geopotential height structure of the Madden–Julian oscillation (MJO) and proposes that the MJO convection signals can be well reflected by upper-tropospheric zonal anomalous height gradient (ZAHG, $$\nabla_{x} z'$$
Jeremy Cheuk-Hin Leung, Weihong Qian
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