Opposing Trends of Winter Cold Extremes over Eastern Eurasia and North America under Recent Arctic Warming

2020 ◽  
Vol 37 (12) ◽  
pp. 1417-1434
Author(s):  
Shuangmei Ma ◽  
Congwen Zhu
2015 ◽  
Vol 96 (5) ◽  
pp. 707-714 ◽  
Author(s):  
Geert Jan Van Oldenborgh ◽  
Rein Haarsma ◽  
Hylke De Vries ◽  
Myles R. Allen

Abstract The winter of 2013–14 had unusual weather in many parts of the world. Here we analyze the cold extremes that were widely reported in North America and the lack of cold extremes in western Europe. We perform a statistical analysis of cold extremes at two representative stations in these areas: Chicago, Illinois, and De Bilt, the Netherlands. This shows that the lowest minimum temperature of the winter was not very unusual in Chicago, even in the current warmer climate. Around 1950 it would have been completely normal. The same holds for multiday cold periods. Only the whole winter temperature was unusual, with a return time larger than 25 years. In the Netherlands, the opposite holds: the absence of any cold waves was highly unusual even now, and would have been extremely improbable halfway through the previous century. These results are representative of other stations in the regions. The difference is due to the skewness of the temperature distribution. In both locations, cold extremes are more likely than equally large warm extremes in winter. Severe cold outbreaks and cold winters, like the winter of 2013–14 in the Great Lakes area, are therefore not evidence against global warming: they will keep on occurring, even if they become less frequent. The absence of cold weather as observed in the Netherlands is a strong signal of a warming trend, as this would have been statistically extremely improbable in the 1950s.


2015 ◽  
Vol 8 (10) ◽  
pp. 759-762 ◽  
Author(s):  
Jong-Seong Kug ◽  
Jee-Hoon Jeong ◽  
Yeon-Soo Jang ◽  
Baek-Min Kim ◽  
Chris K. Folland ◽  
...  

2021 ◽  
Author(s):  
Jennifer Francis ◽  
Natasa Skific ◽  
Stephen Vavrus ◽  
Judah Cohen
Keyword(s):  

2015 ◽  
Vol 96 (9) ◽  
pp. 1489-1503 ◽  
Author(s):  
James A. Screen ◽  
Clara Deser ◽  
Lantao Sun

Abstract In early January 2014, an Arctic air outbreak brought extreme cold and heavy snowfall to central and eastern North America, causing widespread disruption and monetary losses. The media extensively reported the cold snap, including debate on whether human-induced climate change was partly responsible. Related to this, one particular hypothesis garnered considerable attention: that rapid Arctic sea ice loss may be increasing the risk of cold extremes in the midlatitudes. Here we use large ensembles of model simulations to explore how the risk of North American daily cold extremes is anticipated to change in the future, in response to increases in greenhouse gases and the component of that response solely due to Arctic sea ice loss. Specifically, we examine the changing probability of daily cold extremes as (un)common as the 7 January 2014 event. Projected increases in greenhouse gases decrease the likelihood of North American cold extremes in the future. Days as cold or colder than 7 January 2014 are still projected to occur in the mid-twenty-first century (2030–49), albeit less frequently than in the late twentieth century (1980–99). However, such events will cease to occur by the late twenty-first century (2080–99), assuming greenhouse gas emissions continue unabated. Continued Arctic sea ice loss is a major driver of decreased—not increased—North America cold extremes. Projected Arctic sea ice loss alone reduces the odds of such an event by one-quarter to one-third by the mid-twenty-first century, and to zero (or near zero) by the late twenty-first century.


2013 ◽  
Vol 26 (13) ◽  
pp. 4749-4757 ◽  
Author(s):  
Jianping Duan ◽  
Qi-bin Zhang ◽  
Li-Xin Lv

Abstract The recent increase in the frequency of winter cold extremes has received particular attention in light of the climate's warming. Knowledge about changes in the frequency of winter cold extremes requires long-term climate data over large spatial scale. In this study, a temperature-sensitive tree-ring network consisting of 31 sampling sites collected from seven provinces in subtropical China was used to investigate the characteristics of cold-season temperature extremes during the past two centuries. The results show that the percentage of trees in a year that experienced an abnormal decrease in radial growth relative to the previous year can serve as an indicator of interannual change in January–March temperature in subtropical China. The frequency of extreme interannual decreases in cold-season temperature has increased since the 1930s. The change in cold-season temperature was significantly correlated with the intensity of the Siberian high, yet the correlation was much weaker in the period preceding the 1930s. The findings provide evidence of a frequency change in the occurrence of interannual cold-season temperature extremes in the past two centuries for subtropical China. Particularly, the pattern in the variation of cold-season temperature suggests a change in climate systems around the 1930s.


Author(s):  
Marlene Kretschmer ◽  
Judah Cohen ◽  
Vivien Matthias ◽  
Jakob Runge ◽  
Dim Coumou
Keyword(s):  

2021 ◽  
Author(s):  
Dae Il Jeong ◽  
Bin Yu ◽  
Alex J. Cannon

Abstract Due to the significant negative consequences of winter cold extremes, there is need to better understand and simulate the mechanisms driving their occurrence. The impact of atmospheric blocking on winter cold spells over North America is investigated using ERA-Interim and NCEP-DOE-R2 reanalyses for 1981–2010. Initial-condition large-ensembles of two generations of Canadian Earth System Models (CanESM5 and its predecessor, CanESM2) are evaluated in terms of their ability to represent the blocking-cold spell linkage and the associated internal-variability. The reanalysis datasets show that 72% and 58% of cold spells in southern and northern North America coincide with blocking occurring in the high-latitude Pacific-North America. Compared to the two reanalyses, CanESM2 and CanESM5 ensembles underestimate by 19.9% and 14.3% cold spell events coincident with blocking, due to significant under-representation of blocking frequency over the north Pacific (-47.1% and − 29.0%), whereas biases in cold spell frequency are relatively small (6.6% and − 4.7%). In the reanalyses, regions with statistically significant above-normal cold spell frequency relative to climatology lie on the east and/or south flanks of blocking events, whereas those with below-normal frequency lie along the core or surrounding the blocking. The two ensembles reproduce the observed blocking-cold spell linkage over North America, despite underestimating the magnitude of blocking frequency. The two ensembles also reproduce the physical drivers that underpin the blocking-cold spell linkage. Spatial agreement with the reanalyses is found in the simulated patterns of temperature advection and surface heat flux forcing anomalies during blocking events. While CanESM5 shows an improved representation of the blocking climatology relative to CanESM2, both yield similar results in terms of the blocking-cold spell linkage and associated internal-variability.


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