[PDF] Top 20 Impact of CO2 and climate on Last Glacial maximum vegetation – a factor separation
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Impact of CO2 and climate on Last Glacial maximum vegetation – a factor separation
... The factor separation of Stein and Alpert (1993) is applied to simulations with the MPI Earth system model to determine the factors which cause the differences between vegetation patterns in ... See full document
12
Quantifying the effect of vegetation dynamics on the climate of the Last Glacial Maximum
... of vegetation dynamics on air temperature is less important for the LGM climate than the impact of CO 2 changes and the presence of ice sheets, it was shown that in the northern high latitudes of ... See full document
7
Impacts of land surface properties and atmospheric CO 2on the Last Glacial Maximum climate: a factor separation analysis
... 43 Fig. 8. Annual precipitation anomalies (EXPERIMENT-minus-CTRL) for (a) experiment I; (b) experiment O; (c) experiment V; (d) experi- ment C. Only anomalies greater than one standard deviation for the long-term annual ... See full document
20
Influence of dynamic vegetation on climate change and terrestrial carbon storage in the Last Glacial Maximum
... unrealistic vegetation feedback caused by temperature and precipitation ...the climate of the LGM, the vegetation feedback onto the climate and the resul- tant equilibrium carbon storage with ... See full document
17
Tropical climate variability from the last glacial maximum to the present
... [36] In this study, we 'have doubled the previous number of CSEs [King and Repeta, 1994] that can be separated by optimizing the HPLC solvent composition and the columns. By only resolving about half of the CSEs reported ... See full document
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Implications of coral reef buildup for the controls on atmospheric CO2 since the Last Glacial Maximum
... the impact of this occurs during the early Holocene (11 – 8 kyr BP) [Broecker et ...dynamic vegetation models ascribe much of the deglacial increase in terrestrial carbon to a ‘‘CO 2 - fertilization’’ ... See full document
10
The effect of a dynamic soil scheme on the climate of the mid-Holocene and the Last Glacial Maximum
... Using a model of intermediate complexity, Jahn et al. (2005) quantified the single effects of lowering atmo- spheric CO 2 , ice sheets, and vegetation dynamics for the LGM time period. They constrained additional ... See full document
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Skill and reliability of climate model ensembles at the Last Glacial Maximum and mid-Holocene
... future climate, the LGM with its large forcing seems the most promising of the two experiments ...However, climate science is now fac- ing the challenge of predicting future changes on regional scales, ... See full document
13
Responses of basal melting of Antarctic ice shelves to the climatic forcing of the last glacial maximum and CO2 doubling
... important factor in determining the stability of the Antarctic ice ...the Last Glacial Maximum ...to climate warming is much greater (by an order of magnitude) than that due to ...and ... See full document
25
Coupled climate–carbon cycle simulation of the Last Glacial Maximum atmospheric CO2 decrease using a large ensemble of modern plausible parameter sets
... the impact of alternative assumptions regarding parameter values or model ...simulated climate, which is still infrequently done in LGM CO 2 experiments, and the first time it is done with GENIE- ... See full document
24
Vegetation and climate history during the last glacial-interglacial cycle at Lake Van, eastern Anatolia
... the impact of global paleoclimate changes on regional scales are provided by studies on high-resolution paleoarchives from different ...Mediterranean climate to the North Atlantic ocean-atmosphere system ... See full document
123
Climate of the Last Glacial Maximum: sensitivity studies and model-data comparison with the LOVECLIM coupled model
... of Last Glacial Maximum climate simu- lations obtained with the Earth System model LOVECLIM, including coupled dynamic atmosphere, ocean and vegeta- tion ...The climate obtained using ... See full document
20
CiteSeerX — The climate of the Last Glacial Maximum: Results from a coupled atmosphere-ocean general circulation model
... Tropical SST cooling of 4⬚–6⬚C and reduced amounts of atmospheric water vapor combine to cool the tropical atmo- sphere to a degree not previously simulated. SST changes in the tropical Pacific Ocean have the largest ... See full document
18
The last glacial maximum and late glacial environmental and climate dynamics in the Baikal region inferred from an oxygen isotope record of lacustrine diatom silica
... Heavy liquid separation (HLS) with sodium polytungstate (SPT; 3Na 2 WO 4 $9WO 3 $H 2 O) is also used (Morley et al., 2004; Chapligin et al., 2012). Within this study the clean-up procedure involved the process of ... See full document
12
Sea-salt aerosol response to climate change: Last Glacial Maximum, preindustrial, and doubled carbon dioxide climates
... a factor of 2 of the observations, similar to previous studies [Gong et ...a factor of 3 too high relative to the ...a factor of 2 (South Pole) and a factor of 28 (Halley Bay) too ... See full document
11
European emissions of isoprene and monoterpenes from the Last Glacial Maximum to present
... the climate as has occurred since the Last Glacial Maximum, many of the observed vegetation changes can be attributed to this climate ...paleo- climate simulations with ... See full document
19
Modeling Mediterranean Ocean climate of the Last Glacial Maximum
... Abstract. A regional ocean general circulation model of the Mediterranean is used to study the climate of the Last Glacial Maximum. The atmospheric forcing for these sim- ulations has been ... See full document
20
Abrupt climate and vegetation variability of eastern Anatolia during the last glacial
... rapid vegetation and environmental changes can be related to the stadial-interstadial pattern of Dansgaard–Oeschger (DO) events as recorded in the Greenland ice ...the vegetation composition in eastern ... See full document
15
Simulating the Last Glacial Maximum and abrupt glacial climate shifts in a coupled Earth System Model
... Responses of SAT and precipitation to FWP in different models are shown in Figures 5.1 and 5.2. Some regions, i.e. the North Atlantic, the tropical Atlantic and the African and Indian monsoon regions share consistent ... See full document
118
Vegetation and environments since the Last Glacial Maximum in the Southern Tablelands, New South Wales
... Sediments, water content, loss on ignition and charcoal counts for core MS3 at Micalong Swamp. 4 for key to sediments.[r] ... See full document
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