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DOI | 10.1073/pnas.1412797111 |
Quasi-resonant circulation regimes and hemispheric synchronization of extreme weather in boreal summer | |
Coumou D.; Petoukhov V.; Rahmstorf S.; Petri S.; Schellnhuber H.J. | |
发表日期 | 2014 |
ISSN | 0027-8424 |
起始页码 | 12331 |
结束页码 | 12336 |
卷号 | 111期号:34 |
英文摘要 | The recent decade has seen an exceptional number of high-impact summer extremes in the Northern Hemisphere midlatitudes. Many of these events were associated with anomalous jet stream circulation patterns characterized by persistent high-amplitude quasi-stationary Rossby waves. Two mechanisms have recently been proposed that could provoke such patterns: (i) a weakening of the zonal mean jets and (ii) an amplification of quasi-stationary waves by resonance between free and forced waves in midlatitude waveguides. Based upon spectral analysis of the midtroposphere wind field, we show that the persistent jet stream patterns were, in the first place, due to an amplification of quasi-stationary waves with zonal wave numbers 6-8. However, we also detect a weakening of the zonal mean jet during these events; thus both mechanisms appear to be important. Furthermore, we demonstrate that the anomalous circulation regimes lead to persistent surface weather conditions and therefore to midlatitude synchronization of extreme heat and rainfall events on monthly timescales. The recent cluster of resonance events has resulted in a statistically significant increase in the frequency of high-amplitude quasi-stationary waves of wave numbers 7 and 8 in July and August. We show that this is a robust finding that holds for different pressure levels and reanalysis products. We argue that recent rapid warming in the Arctic and associated changes in the zonal mean zonal wind have created favorable conditions for double jet formation in the extratropics, which promotes the development of resonant flow regimes. |
英文关键词 | Arctic amplification; Climate change; Climate impact; Midlatitude weather; Planetary waves |
语种 | 英语 |
scopus关键词 | rain; altitude; article; controlled study; heat; Northern Hemisphere; priority journal; Southern Hemisphere; summer; surface property; wind |
来源期刊 | Proceedings of the National Academy of Sciences of the United States of America
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/158917 |
作者单位 | Coumou, D., Potsdam Institute for Climate Impact Research, 14412 Potsdam, Germany; Petoukhov, V., Potsdam Institute for Climate Impact Research, 14412 Potsdam, Germany; Rahmstorf, S., Potsdam Institute for Climate Impact Research, 14412 Potsdam, Germany; Petri, S., Potsdam Institute for Climate Impact Research, 14412 Potsdam, Germany; Schellnhuber, H.J., Potsdam Institute for Climate Impact Research, 14412 Potsdam, Germany, Santa Fe Institute, Santa Fe, NM 87501, United States |
推荐引用方式 GB/T 7714 | Coumou D.,Petoukhov V.,Rahmstorf S.,et al. Quasi-resonant circulation regimes and hemispheric synchronization of extreme weather in boreal summer[J],2014,111(34). |
APA | Coumou D.,Petoukhov V.,Rahmstorf S.,Petri S.,&Schellnhuber H.J..(2014).Quasi-resonant circulation regimes and hemispheric synchronization of extreme weather in boreal summer.Proceedings of the National Academy of Sciences of the United States of America,111(34). |
MLA | Coumou D.,et al."Quasi-resonant circulation regimes and hemispheric synchronization of extreme weather in boreal summer".Proceedings of the National Academy of Sciences of the United States of America 111.34(2014). |
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