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表1 IPCC第五次與第六次報(bào)告兩套人類排放情景貢獻(xiàn)2100年年度人為排放[1]

Table 1 Two human emission scenarios contributed to 2100 for AR5 and AR6 [1]

表2 2081—2100年相對(duì)于1850—1900年在SSP不同排放情景下人類活動(dòng)對(duì)全球氣溫的貢獻(xiàn)[1]

Table 2 Contributions of different emission scenarios to temperature for 2081-2100 relative to 1850-1900 [1]

表3 IPCC各次報(bào)告2100年人為排放情景對(duì)應(yīng)化石燃料和工業(yè)CO2排放對(duì)比以及對(duì)應(yīng)敏感平衡溫度和未來(lái)預(yù)估21世紀(jì)后期溫度變化（相對(duì)于目前氣候）[1-2]

Table 3 Comparisons of anthropogenic emission scenarios corresponding to fossil fuel and industrial carbon dioxide emission in 2100, equilibrium climate sensitivity, and projected temperature changes in the late 21st century (relative to present time) [1-2]

表4 常用5套觀測(cè)資料的一致性對(duì)比：2023年（1—10月）全球平均溫度相對(duì)于4個(gè)基準(zhǔn)時(shí)段的距平[3]

Table 4 Comparison of consistency of global mean temperature anomalies for 2023 (January - October) relative to four different baselines of five traditional observation datasets [3]

表5 從第一次IPCC報(bào)告到第六次報(bào)告全球氣候模式的發(fā)展[1]

Table 5 Developments of global climate models from IPCC FAR to AR6 [1]

表6 過(guò)去、現(xiàn)在和未來(lái)3個(gè)時(shí)段大氣CO2濃度，以及全球溫度和全球海平面高度的變化[1]

Table 6 Atmospheric carbon dioxide concentrations for three periods, global temperature, and global sea level during present-day (2011-2020), and future (2100) under low-emissions scenarios (SSP1-2.6) and very high-emissions scenarios (SSP5-8.5) as compared to 1850-1900[1]