Part of variables from GCM experiments on the last interglacial using MIROC4m and MIROC4m-LPJ

This data is used in the paper O'ishi, R., Chan, W.-L., Abe-Ouchi, A., Sherriff-Tadano, S., Ohgaito, R. and Yoshimori, M.: PMIP4/CMIP6 Last Interglacial simulations using three different versions of MIROC: importance of vegetation, Clim. Past, in press, 2020. (1) insolation difference between 127ka and pre-industrial. (2) vegetaion distribution used in Figure 2. (3) Temperature, precipitation and sea-ice in 127ka and pre-industrial obtained from MIROC4m and MIROC4m-LPJ. (4) result of feedback analysis for Figure 16. All data are monthly climatlogy.本数据集用于论文：O'ishi, R.、Chan, W.-L.、Abe-Ouchi, A.、Sherriff-Tadano, S.、Ohgaito, R. 与 Yoshimori, M.：《使用MIROC三个不同版本的PMIP4/CMIP6末次间冰期模拟：植被的重要性》，《气候往事》（Climate of the Past），已接收待刊，2020年。 (1) 127千年前与工业化前时期的日照辐射差值 (2) 图2中所用的植被分布数据 (3) 由MIROC4m与MIROC4m-LPJ模拟得到的127千年前及工业化前时期的气温、降水与海冰数据 (4) 图16对应的反馈分析结果 所有数据均为逐月气候态。