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Lijing Cheng, Gongjie Wang, John P. Abraham and Gang Huang
Ocean heat content (OHC) is the major component of the earth’s energy imbalance. Its decadal scale variability has been heavily debated in the research interest of the so-called “surface warming slowdown” (SWS) that occurred during the ...
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Ka-Kit Tung and Xianyao Chen
The Intergovernmental Panel on Climate Change (IPCC) noted a recent 15-year period (1998–2012) when the rate of surface global warming was a factor of 4 smaller than the mean of the state-of-art climate model projections and than that observed in t...
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Norman G. Loeb, Tyler J. Thorsen, Joel R. Norris, Hailan Wang and Wenying Su
This study examines changes in Earth’s energy budget during and after the global warming “pause” (or “hiatus”) using observations from the Clouds and the Earth’s Radiant Energy System. We find a marked 0.83 ± 0....
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Kristoffer Rypdal
The main features of the instrumental global mean surface temperature (GMST) are reasonably well described by a simple linear response model driven by anthropogenic, volcanic and solar forcing. This model acts as a linear long-memory filter of the forcin...
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Knut L. Seip and Hui Wang
Ocean oscillations interact across large regions and these interactions may explain cycles in global temperature anomaly, including hiatus periods. Here, we examine ocean interaction measures and compare results from model simulations to observations for...
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Yukiko Imada, Shuhei Maeda, Masahiro Watanabe, Hideo Shiogama, Ryo Mizuta, Masayoshi Ishii and Masahide Kimoto
Since the late 1990s, land surface temperatures over Japan have increased during the summer and autumn, while global mean temperatures have not risen in this duration (i.e., the global warming hiatus). In contrast, winter and spring temperatures in Japan...
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