Carbon dioxide and the δ18O record of late-Quaternary climatic change: a global model Barry Saltzman OriginalPaper Pages: 77 - 85
The influence of continental ice, atmospheric CO2, and land albedo on the climate of the last glacial maximum A J BroccoliS Manabe OriginalPaper Pages: 87 - 99
Reconstruction of the last deglaciation: deconvolved records of δ18O profiles, micropaleontological variations and accelerator mass spectrometric14C dating E BardM ArnoldJ-C Duplessy OriginalPaper Pages: 101 - 112
Interannual variability of the simulated hydrology in a climatic model-implications for drought HB GordonBG Hunt OriginalPaper Pages: 113 - 130