Vertical heat transports in the ocean and their effect on time-dependent climate change

By J. Gregory. 2000

313 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/8a262e8fd64c22e4f14bab4cb6f529a36fbf3bc8

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Citations in the corpus

Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “…and troposphere (days to weeks), fast responses of the land surface and the ocean’s mixed layer (months to years), and a long-term adjustment of the deeper ocean (decades to millennia) [e.g., Gregory, 2000; Stouffer, 2004; Gregory and Webb, 2008; Held et al., 2010; Andrews et al., 2012].”
The Role of Climate Sensitivity and Ocean Heat Uptake on AOGCM Transient Temperature Response (2002, background): “In high latitudes, the increased stability of the oceans resulting from surface warming and freshening inhibits heat loss from the interior of the ocean [by convection and upward diffusion along surfaces of constant density; Osborn (1998); Gregory (2000)].”
Transient Climate Response in a Two-Layer Energy-Balance Model. Part I: Analytical Solution and Parameter Calibration Using CMIP5 AOGCM Experiments (2013, background): “(2002) and Gregory and Forster (2008) and of the same order of magnitude as the estimates of Plattner et al.”
Impact of the Atlantic meridional overturning circulation on ocean heat storage and transient climate change (2014, background): “Gregory, M. J. Webb, and K. E. Taylor (2012), Forcing, Feedbacks and Climate Sensitivity in CMIP5 Coupled Atmosphere-Ocean Climate Models, Geophys. Res. Lett., 39 (9), L09712, doi:10.1029/2012GL051607. Armour, K. C., C. M. Bitz, and G. H. Roe (2013), Time-Varying Climate Sensitivity from Regional Fe”
Loss of cultural world heritage and currently inhabited places to sea-level rise (2014, background): “Keywords: sea-level rise, cultural heritage, chlimate impacts S Online supplementary data available from stacks.iop.org/ERL/9/034001/mmedia”
OMIP contribution to CMIP6: experimental and diagnostic protocol for the physical component of the Ocean Model Intercomparison Project (2016, background): “…has a particular interest in the detailed workings of mesoscale eddy parameterizations, particularly as they impact on vertical heat transport (e.g. Gregory, 2000), and the response of the Antarctic Circumpolar Current (ACC) and Southern Ocean meridional overturning circulation (MOC) to changes in…”
The dependence of transient climate sensitivity and radiative feedbacks on the spatial pattern of ocean heat uptake (2014, background): “…the spatial pattern of ocean2 heat uptake3 Brian E. J. Rose, 1 Kyle C. Armour, 2 David S. Battisti, 3 Nicole Feldl 4 and Daniel D. B. Koll 5 Corresponding author: B. Rose, Department of Atmospheric and Environmental Sciences, University at Albany, ES 351, 1400 Washington Ave., Albany, NY 12222,…”
Antarctic climate response to stratospheric ozone depletion in a fine resolution ocean climate model (2012, result): “In spite of these differences, and although the area of significant surface warming is larger in the 1 case, we obtain the surprising results that the total annual loss of Antarctic SIE is nearly independent of resolution, at 0.77 106 km2 in the 0.1 case and 0.85 106 km2 in the 1 case.”
Time-Varying Climate Sensitivity from Regional Feedbacks (2012, background): “face cooling due to reduced upward isopycnal mixing of heat into the ocean mixed layer (Gregory 2000; Kirkman and Bitz 2011); and increased ocean heat transport into the Arctic Ocean enhances sea ice loss and local surface warming (Holland et al.”
Deep-ocean heat uptake and equilibrium climate response (2013, methodology): “The slow surface warming over these domains is related to the DOHU (Gregory 2000).”
The ocean’s role in the transient response of climate to abrupt greenhouse gas forcing (2015, background): “It has been argued that the delayed surface warming and sea ice expansion around Antarctica is the result of deep J. Marshall (*) · K. C. Armour · J.-M. Campin Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA e-mail: jmarsh@mit.edu J.”