Tropical cooling and the isotopic composition of precipitation in general circulations model simulations of the ice age climate

Climate Dynamics

Volumn 17, Issue 7, 2001, Pages 489-502

  Charles, C D ^a   Rind, D ^a   Healy, R ^a   Webb, R ^a  

^a UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

GENERAL CIRCULATION MODEL; ISOTOPIC ANALYSIS; PALEOCLIMATE; PRECIPITATION QUALITY; SEA SURFACE TEMPERATURE;

EID: 0034826729     PISSN: 09307575     EISSN: 14320894     Source Type: Journal    
DOI: 10.1007/s003820000126     Document Type: Article

References (43)

1. Interhemispheric synchrony of the last deglaciation inferred from alkenon palaeothermometry
2. Abrupt changes in early Holocene tropical sea surface temperature derived from coral records
3. Cool tropical temperatures shift the global delta O-18-T relationship: An explanation for the ice core delta O-18-borehole thermometry conflict?
4. Ice cores - Cooling the tropics
5. The role of ocean atmosphere reorganizations in glacial cycles
6. The role of ocean-atmosphere interactions in tropical cooling during the last glacial maximum
7. Climate change - A role for the tropical Pacific
8. The surface of the ice age earth
9. Nature of environmental changes in South America at the last glacial maximum
10. Climatic controls on interannual variability of precipitation delta O-18: Simulated influence of temperature, precipitation amount, and vapor source region
11. A new estimate of the Holocene low stand level of Lake Titicaca
12. Large Arctic temperature change at the Wisconsin-Holocene glacial transition
13. Stable isotopes in precipitation
14. Simulation of modern and glacial climates with a coupled global model of intermediate complexity
15. Tropical temperature variations since 20 000 years ago: Modulating interhemispheric climate change
16. The maintenance of the last great ice sheets - A UGAMP GCM study
17. Efficient three-dimensional global models for climate studies, models I and II
18. Climate sensitivity: Analysis of feedback mechanisms
19. Reassessment of ice-age cooling of the tropical ocean and atmosphere
20. Simulations of the HDO and (H2O)-O-18 atmospheric cycles using the Nasa Giss general circulation model-sensitivity experiments for present-day conditions
21. Simulations of the HDO and H218O atmospheric cycles using the NASA GISS general circulation model: The seasonal cycle for present-day conditions
22. Global sources of local precipitation as determined by the NASA/GISS GCM
23. Absence of last glacial maximum records in lowland tropical forests
24. The influence of vegetation on the hydrologic cycle in a global climate model
25. The dynamics of warm and cold climates
26. Components of the ice age circulation
27. Dependence of warm and cold climate depiction on climate model resolution
28. Latitudinal temperature gradients and climate change
29. Terrestrial conditions at the last glacial maximum and CLIMAP sea-surface temperature estimates: Are they consistent?
30. Can Milankovitch orbital variations initiate the growth of ice sheets in a general circulation model?
31. Reconstructing sea surface temperature and salinity using delta-o-18 and alkenone records
32. Sand deserts during the glacial maximum and climatic optimum
33. Timing of abrupt climate change at the end of the younger dryas interval from thermally fractionated gases in polar ice
34. Tropical forest changes during the late quaternary in African and South American lowlands
35. Global maps of lake-level fluctuations since 30 000 yr BP
36. Cooling of tropical Brazil (5 °C) during the last glacial maximum
37. Late glacial stage and holocene tropical ice core records from Huascaran, Peru
38. Tropical climate instability: The last glacial cycle from a Qinghai-Tibetan ice core
39. A 25 000-year tropical climate history from Bolivian ice cores
40. Teleconnections in the geopotential height field during the Northern Hemisphere winter season
41. Simulated influence of carbon dioxide, orbital forcing, and ice sheets on the climate of the last glacial maximum
42. Influence of ocean heat transport on the climate of the last glacial maximum