When the sea-surface temperature (SST) and the land- plus-ocean surface temperature (ST) are averaged globally to yield the global-mean SST (GSST) and the GST, respectively, spatial information is lost. Information on both space and time is needed to properly identify the modes of ...
We have produced a revised set of global and hemispheric mean surface temperature reconstructions for past centuries using a newly developed network of long-term climate proxy data. Three alternative statistical approaches that have been tested and validated in long-term climate model simulation experimen...
The CMIP5 ensemble-meanTshows a sudden global-mean cooling of 0.1–0.3 K caused by the negative forcing from each historical volcanic eruption (Fig.2a). The observedTtimeseries has larger interannual variability, because unforced interannual variability is independent in each model; the interannual s...
[1] Trends and interannual variability of the surface winds (SW), sea surface height (SSH), and sea surface temperature (SST) of the South China Sea (SC... G Fang,H Chen,Z Wei,... - 《Journal of Geophysical Research Oceans》 被引量: 306发表: 2006年 Variations in global mean sea ...
4). At the thousands of sites surveyed, the mean SST recorded during coral bleaching in the first decade of the dataset, from 1998 to 2006, was 28.1 °C, whereas the mean SST recorded during coral bleaching in the second decade, from 2007 to 2017, was 28.7 °C. This change ...
and the minimum value for the day), expressed as a percentage of the mean daily PEF value, and averaged over 1-2 weeks19. Another method of describing PEF variability is the minimum morning pre-bronchodilator PEF over 1 week, expressed as a percent of the recent best (Min%Max) (Figure ...
et al. The mean climate of the Community Atmosphere Model (CAM4) in forced SST and fully coupled experiments. J. Clim. 26, 5150–5168 (2013). Article ADS Google Scholar Bitz, C. M. et al. Climate sensitivity of the community climate system model, version 4. J. Clim. 25, 3053–...
Local- and regional-scale heat extremes can increase at a significantly greater rate than global mean changes, presenting challenges for human health, infrastructure, industry and ecosystems. We examine changes in regional absolute temperature extremes for a suite of global regions under 1.5 °C and...
Individual sea surface temperature (SST) anomalies are calculated using a satellite-based climatology and observations from the World Ocean Atlas 1994 (WOA... KS Casey,P Cornillon - 《J Clim》 被引量: 5469发表: 2001年 The 1998 Oklahoma–Texas Drought: Mechanistic Experiments with NCEP Global and...
Significant changes of mean state appearing widely in the global sea-surface temperature (SST) anomaly field have happened five times from the 1910s to the 1990s: 1925, 1942, 1957, 1970 and 1976. Since the regions of change spread over both hemispheres and/or multiple oceanic basins, they ca...