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Mass distribution and mass transport in the Earth system
Institution:1. Development Research Centre, China Geological Survey, Beijing 100037, PR China;2. School of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, PR China;1. School of Cyber Science and Technology, Beihang University, China;2. National Computer Network Emergency Response Technical Team/Coordination Center of China, China;3. School of Information, Beijing Wuzi University, China;4. School of Computer Science and Technology, Nanjing University of Aeronautics and Astronautics, 210016, China;5. Beijing Key Laboratory of Network Technology, Beihang University, Beijing 100191, China;1. A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia;2. V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia;3. Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia;4. Siberian Research Institute of Geology, Geophysics, and Mineral Deposits, Krasnyi pr. 67, Novosibirsk, 630091, Russia;1. Sultan Qaboos University, Muscat, Oman;2. Institute of Geophysics, University of Tehran, Tehran, Iran
Abstract:Melting of continental ice sheets and glaciers, changes in ocean circulation pattern and in sea level, variations of surface and ground water levels and river discharge, glacial-isostatic adjustment, mantle convection and tectonics, all this causes transport and (re-) distribution of mass inside the Earth and at its surface. Equipped with precise sensor systems, gravity field and altimeter satellites observe these mass-transport processes. During 2006–2012, the German Research Association DFG had established the SPP 1257, ‘Mass distribution and Mass Transport in the Earth System’ as a coordinated research programme to facilitate integrated analysis of these data, to improve our knowledge about several transport processes within the Earth system and to investigate their interactions. This special issue reports about the findings of the first 4 years within the programme.
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