id	author	title	date	pages	extension	mime	words	sentences	flesch	summary	cache	txt
work_nrii46c64fc77ehgikuwgdsplu	Robert J. Wasson	Earth system models: a test using the mid-Holocene in the Southern Hemisphere	2002	6	.pdf	application/pdf	3601	264	57	Palaeoclimatic reconstructions from proxy data have been compared with climate model outcomes for three decades. (CLIMBER) and proxy data from Southern Hemisphere locations to compare postdictions of mid-Holocene climates. Global, hemispheric and regional syntheses of palaeoclimate reconstructions for different periods of the Late climate change have come slowly as models of the ocean temperature and sea ice in modulating (particularly amplifying) insolation changes (Ganopolski et al., Differences in boreal winter (December, January, February) mean temperatures between mid-Holocene (6000 years before present) and preindustrial climate. Differences in boreal winter (December, January, February) mean precipitation between mid-Holocene (6000 years before present) and preindustrial climate. Mid-Holocene insolation changes alone (AO) produce a global annual precipitation increase caused At 6 kya, in the southern Andes at least, climate Holocene climate changes. synchronicity of climate change in the two hemispheres. Climatic changes of the last 18,000 years: Observations and model simulations.	./cache/work_nrii46c64fc77ehgikuwgdsplu.pdf	./txt/work_nrii46c64fc77ehgikuwgdsplu.txt