Climate change in the 21st century simulated by HadGEM2-AO under representative concentration pathways

• Published in: Asia-Pacific journal of atmospheric sciences 2013, 49(5), , pp.603-618
• Main Authors: Baek, Hee-Jeong, Lee, Johan, Lee, Hyo-Shin, Hyun, Yu-Kyung, Cho, ChunHo, Kwon, Won-Tae, Marzin, Charline, Gan, Sun-Yeong, Kim, Min-Ji, Choi, Da-Hee, Lee, Jonghwa, Lee, Jaeho, Boo, Kyung-On, Kang, Hyun-Suk, Byun, Young-Hwa
• Format: Article
• Language: English
• Subjects: Atmospheric Sciences; Climatology; Earth and Environmental Science; Earth Sciences; Geophysics/Geodesy; Marine; 대기과학
• ISSN: 1976-7633; 1976-7951
• DOI: 10.1007/s13143-013-0053-7

We present climate responses of Representative Concentration Pathways (RCPs) using the coupled climate model HadGEM2-AO for the Coupled Model Intercomparison Project phase 5 (CMIP5). The RCPs are selected as standard scenarios for the IPCC Fifth Assessment Report and these scenarios include time paths for emissions and concentrations of greenhouse gas and aerosols and land-use/land cover. The global average warming and precipitation increases for the last 20 years of the 21st century relative to the period 1986-2005 are +1.1°C/+2.1% for RCP2.6, +2.4°C/+4.0% for RCP4.5, +2.5°C/+3.3% for RCP6.0 and +4.1°C/+4.6% for RCP8.5, respectively. The climate response on RCP 2.6 scenario meets the UN Copenhagen Accord to limit global warming within two degrees at the end of 21st century, the mitigation effect is about 3°C between RCP2.6 and RCP8.5. The projected precipitation changes over the 21st century are expected to increase in tropical regions and at high latitudes, and decrease in subtropical regions associated with projected poleward expansions of the Hadley cell. Total soil moisture change is projected to decrease in northern hemisphere high latitudes and increase in central Africa and Asia whereas near-surface soil moisture tends to decrease in most areas according to the warming and evaporation increase. The trend and magnitude of future climate extremes are also projected to increase in proportion to radiative forcing of RCPs. For RCP 8.5, at the end of the summer season the Arctic is projected to be free of sea ice.