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Effects on the Earths shape due to ocean mass redistributions from GRACE observations in a warming climate






Geophysical Research Abstracts 11

Effects on the Earths shape due to ocean mass redistributions from GRACE observations in a warming climate



Accession: 037042101



Related references

Chambers Don P.; Tamisiea Mark E.; Nerem R.S.even; Ries John C., 2007: Effects of ice melting on GRACE observations of ocean mass trends. The Gravity Recovery and Climate Experiment (GRACE) was designed to measure variations in the Earth's gravity field from space at monthly intervals. Researchers have used these data to measure changes in water mass over various regions, inclu...

Don P.C.ambers; John Wahr; R.S.even Nerem, 2004: Preliminary observations of global ocean mass variations with GRACE. Geophysical Research Letters 31(13)

L.S.oane; R.B.ancale; D.G.mbis, 2012: Agreement between Earths rotation and mass displacement as detected by GRACE. The progress in GRACE data processing should improve the estimation of low degree spherical harmonics which are expected to agree better with Earth's rotation observations. The polar motion and length-of-day excitations determined from the sp...

Rietbroek, R.; Brunnabend, S.E.; Dahle, C.; Kusche, J.; Flechtner, F.; Schroeter, J.; Timmermann, R., 2009: Changes in total ocean mass derived from GRACE, GPS, and ocean modeling with weekly resolution. We derive changes in ocean bottom pressure (OBP) and ocean mass by combining modeled ocean bottom pressure, weekly GRACE-derived models of gravity change, and large-scale deformation patterns sensed by a global network of GPS stations in a joint l...

Steffen, H.; Wu, P.; Wang, H., 2010: Determination of the Earths structure in Fennoscandia from GRACE and implications for the optimal post-processing of GRACE data. Analysis of data from the Gravity Recovery and Climate Experiment (GRACE) satellite mission allows us to identify regions of long-term mass changes such as the areas of Glacial Isostatic Adjustment (GIA) in North America and Fennoscandia. As there...

Shin-Chan Han; Christopher Jekeli; C.K.S.um, 2004: Time-variable aliasing effects of ocean tides, atmosphere, and continental water mass on monthly mean GRACE gravity field. Journal of Geophysical Research: Solid Earth 109(B4)

Kerr, R.A., 1986: Greenhouse Warming still Coming: Estimates of the carbon dioxide-induced climate warming predict a large effect that could be doubled by increasing trace gases; some effects of the warming may already be evident. Science 232(4750): 573-574

Lal, M.; Bhaskaran, B., 1993: Impact of greenhouse warming on the climate of north-west India as inferred from a coupled atmosphere-ocean climate model. A set of three time-dependent greenhouse warming simulations (the Intergovernmental Panel on Climate Change's (IPCC) scenarios A and D and a sudden increase in carbon dioxide) and a reference control experiment have been performed with the Ha...

Song, Y.T.ny; Colberg, F., 2011: Deep ocean warming assessed from altimeters, Gravity Recovery and Climate Experiment, in situ measurements, and a non-Boussinesq ocean general circulation model. Observational surveys have shown significant oceanic bottom water warming, but they are too spatially and temporally sporadic to quantify the deep ocean contribution to the present-day sea level rise (SLR). In this study, altimetry sea surface hei...

Bottjer, David J., 2011: The end-Permian mass extinction ocean as a model for the future global warming ocean. The Earth is currently warming, largely due to carbon dioxide emissions from the burning of fossil fuels, including coal-fired power plants. The Permian-Triassic transition experienced significantly increased warming due to eruption of a large ign...