Last Glacial Maximum and Holocene Climate in CCSM3

By B. Otto‐Bliesner, E. Brady, G. Clauzet, R. Tomas, Sam Levis, Zavareh Kothavala. 2006

608 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/1e5e02902419499adb3e48e8952d17cc78c565ec

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Citations in the corpus

Integrating ensemble species distribution modelling and statistical phylogeography to inform projections of climate change impacts on species distributions (2013, methodology): “CCSM 3 model (Otto-Bliesner et al. 2006): Global monthly values for all four variables were downloaded from the PMIP 2 database for 0, 6, and 21 kya.”
The use of the multi-model ensemble in probabilistic climate projections (2007, methodology): “They are evaluated against proxy data from past climate states, e.g. the Last Glacial Maximum, the Mid-Holocene, the last Interglacial period, or even further back in time (e.g. Kiehl & Shields 2005; Otto-Bliesner et al. 2006a,b).”
European seaweeds under pressure: Consequences for communities and ecosystem functioning (2015, background): “In opposition, during interglacial periods, such as the Holocene (~12 ka to present-time) we are currently experiencing, the warming climate and retreat of ice sheets led populations to expand from periglacial or southern refugia and colonize the northern European shores (Otto-Bliesner et al., 2006;”
Astronomical and glacial forcing of East Asian summer monsoon variability (2015, unknown): “…and reconstructed precipitation changes in East Asia suggests that the CCSM3 (a coupled ocean-atmosphere model) can be applied well for simulating the seasonal cycle of monsoon circulation and precipitation in East Asia (Meehl et al., 2006; Otto-Bliesner et al., 2006; Braconnot et al., 2007).”
High plant endemism in China is partially linked to reduced glacial‐interglacial climate change (2016, methodology): “The LGM MAT and MAP were computed from the mean of the Community Climate System Model version 3 (CCSM3) (Hijmans et al., 2005; Otto-Bliesner et al., 2006) and Model for Interdisciplinary Research on Climate version 3.2 (MIROC3.”
Gustiness: The driver of glacial dustiness? (2009, methodology): “8 (T42) horizontal resolution were sampled each 12 h in 50year runs forced by sea surface temperatures from CCSM3 simulations of LGM and PI climates (Otto-Bliesner et al., 2006).”
Centennial-scale climate change from decadally-paced explosive volcanism: a coupled sea ice-ocean mechanism (2011, methodology): “CCSM has been used extensively for paleoclimate studies (e.g., Otto-Bliesner et al. 2006a, b; Liu et al. 2009; Kaufman et al. 2009) as well as twentieth and twenty-first century simulations (e.g., Meehl et al. 2006; Holland et al. 2006a).”
The modern and glacial overturning circulation in the Atlantic ocean in PMIP coupled model simulations (2006, methodology): “One of these models shows a salinity increase of glacial AABW at its source region (CCSM), one a freshening of glacial NADW at its source region (UTor) and one seems to be driven by the combined effect of northern freshening and southern salinification during the LGM (ClimC).”