|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Arctic Sea Ice and Eurasian Climate:A Review显示文摘The Arctic plays a fundamental role in the climate system and has shown significant climate change in recent decades,including the Arctic warming and decline of Arctic sea-ice extent and thickness. In contrast to the Arctic warming and reduction of Arctic sea ice, Europe, East Asia and North America have experienced anomalously cold conditions, with record snowfall during recent years. In this paper, we review current understanding of the sea-ice impacts on the Eurasian climate.Paleo, observational and modelling studies are covered to summarize several major themes, including: the variability of Arctic sea ice and its controls; the likely causes and apparent impacts of the Arctic sea-ice decline during the satellite era,as well as past and projected future impacts and trends; the links and feedback mechanisms between the Arctic sea ice and the Arctic Oscillation/North Atlantic Oscillation, the recent Eurasian cooling, winter atmospheric circulation, summer precipitation in East Asia, spring snowfall over Eurasia, East Asian winter monsoon, and midlatitude extreme weather; and the remote climate response(e.g., atmospheric circulation, air temperature) to changes in Arctic sea ice. We conclude with a brief summary and suggestions for future research. | GAO Yongqi SUN Jianqi LI Fei HE Shengping Stein SANDVEN YAN Qing ZHANG Zhongshi Katja LOHMANN Noel KEENLYSIDE Tore FUREVIK SUO Lingling | 2015 | Advances in Atmospheric Sciences2015，32，1： | 21 |
| 2 | Teleconnection between Sea Ice in the Barents Sea in June and the Silk Road,Pacific–Japan and East Asian Rainfall Patterns in August显示文摘In contrast to previous studies that have tended to focus on the influence of the total Arctic sea-ice cover on the East Asian summer tripole rainfall pattern, the present study identifies the Barents Sea as the key region where the June sea-ice variability exerts the most significant impacts on the East Asian August tripole rainfall pattern, and explores the teleconnection mechanisms involved. The results reveal that a reduction in June sea ice excites anomalous upward air motion due to strong near-surface thermal forcing, which further triggers a meridional overturning wave-like pattern extending to midlatitudes.Anomalous downward motion therefore forms over the Caspian Sea, which in turn induces zonally oriented overturning circulation along the subtropical jet stream, exhibiting the east–west Rossby wave train known as the Silk Road pattern. It is suggested that the Bonin high, a subtropical anticyclone predominant near South Korea, shows a significant anomaly due to the eastward extension of the Silk Road pattern to East Asia. As a possible descending branch of the Hadley cell, the Bonin high anomaly ultimately triggers a meridional overturning, establishing the Pacific–Japan pattern. This in turn induces an anomalous anticyclone and cyclone pair over East Asia, and a tripole vertical convection anomaly meridionally oriented over East Asia. Consequently, a tripole rainfall anomaly pattern is observed over East Asia. Results from numerical experiments using version 5 of the Community Atmosphere Model support the interpretation of this chain of events. | Shengping HE Yongqi GAO Tore FUREVIK Huijun WANG Fei LI | 2018 | Advances in Atmospheric Sciences2018，35，1： | 9 |
| 3 | Teleconnection between Winter Arctic Oscillation and Southeast Asian Summer Monsoon in the Pre-Industry Simulation of a Coupled Climate Model显示文摘A 600-year pre-industrial simulation with Bergen Climate Model(BCM)Version 2 is used to investigate the linkage between winter Arctic Oscillation(AO)and the Southeast Asian summer monsoon(SEASM)on the inter-decadal timescale.The results indicate an in-phase relationship between the AO and SEASM with periods of approximately 16–32 and 60–80 years.During the positive phase of winter AO,an anomalous surface anti-cyclonic atmosphere circulation appears over North Pacific in winter.The corresponding anomalies in ocean circulation and surface heat flux,particularly the latent and sensible heat flux,resemble a negative Pacific Decadal Oscillation(PDO)-like sea surface temperature(SST)pattern.The AO-associated PDO-like winter SST can persist into summer and can therefore lead to inter-decadal variability of summer monsoon rainfall in East and Southeast Asia. | CUI Xue-Dong GAO Yong-Qi GONG Dao-Yi GUO Dong Tore FUREVIK | 2013 | Atmospheric and Oceanic Science Letters2013，6，5： | 3 |
| 4 | Air–Sea Coupling Enhances the East Asian Winter Climate Response to the Atlantic Multidecadal Oscillation显示文摘A simple air–sea coupled model,the atmospheric general circulation model(AGCM) of the National Centers for Environmental Prediction coupled to a mixed-layer slab ocean model,is employed to investigate the impact of air–sea coupling on the signals of the Atlantic Multidecadal Oscillation(AMO). A regional coupling strategy is applied,in which coupling is switched off in the extratropical North Atlantic Ocean but switched on in the open oceans elsewhere. The coupled model is forced with warm-phase AMO SST anomalies,and the modeled responses are compared with those from parallel uncoupled AGCM experiments with the same SST forcing. The results suggest that the regionally coupled responses not only resemble the AGCM simulation,but also have a stronger intensity. In comparison,the coupled responses bear greater similarity to the observational composite anomaly. Thus,air–sea coupling enhances the responses of the East Asian winter climate to the AMO. To determine the mechanism responsible for the coupling amplification,an additional set of AGCM experiments,forced with the AMO-induced tropical SST anomalies,is conducted. The SST anomalies are extracted from the simulated AMO-induced SST response in the regionally coupled model. The results suggest that the SST anomalies contribute to the coupling amplification. Thus,tropical air–sea coupling feedback tends to enhance the responses of the East Asian winter climate to the AMO. | ZHOU Xiaomin LI Shuanglin LUO Feifei GAO Yongqi Tore FUREVIK | 2015 | Advances in Atmospheric Sciences2015，32，12： | 3 |
| 5 | A New Method for Predicting the Decadal Component of Global SST显示文摘A simple approach that considers both internal decadal variability and the effect of anthropogenic forcing is developed to predict the decadal components of global sea surface temperatures (SSTs) for the three decades 2011-2040. The internal decadal component is derived by harmonic wave expansion analyses based on the quasiperiodic evolution of the Pacific Decadal Oscillation (PDO) and the Atlantic Multidecadal Oscillation (AMO), as obtained from observational SST datasets. Furthermore, the external decadal component induced by anthropogenic forcing is assessed with a second-order fit based on the ensemble of projected SSTs in the experiments with multiple coupled climate models associated with the third Coupled Model Intercomparison Project (CMIP3) under the Intergovernmental Panels on Climate Change (IPCC) Special Reports on Emissions Scenario (SRES) A1B. A validation for the years from 2002 to 2010 based on a comparison of the predicted and the observed SST and their spatial correlation, as well as the root mean square error (RMSE), suggests that the approach is reasonable overall. In addition, the predicted results over the 50°S-50°N global band, the Indian Ocean, the western Pacific Ocean, the tropical eastern Pacific Ocean, and the North and the South Atlantic Ocean are presented. | LUO Fei-Fei LI Shuanglin GAO Yong-Qi Tore FUREVIK | 2012 | Atmospheric and Oceanic Science Letters2012，5，6： | 3 |
| 6 | Simulation by CMIP5 Models of the Atlantic Multidecadal Oscillation and Its Climate Impacts显示文摘This study focuses on the climatic impacts of the Atlantic Multidecadal Oscillation(AMO) as a mode of internal variability. Given the difficulties involved in excluding the effects of external forcing from internal variation, i.e., owing to the short record length of instrumental observations and historical simulations, we assess and compare the AMO and its related climatic impacts both in observations and in the 'Pre-industrial' experiments of models participating in CMIP5. First, we evaluate the skill of the 25 CMIP5 models' 'Historical' simulations in simulating the observational AMO, and find there is generally a considerable range of skill among them in this regard. Six of the models with higher skill relative to the other models are selected to investigate the AMO-related climate impacts, and it is found that their 'Pre-industrial' simulations capture the essential features of the AMO. A positive AMO favors warmer surface temperature around the North Atlantic,and the Atlantic ITCZ shifts northward leading to more rainfall in the Sahel and less rainfall in Brazil. Furthermore, the results confirm the existence of a teleconnection between the AMO and East Asian surface temperature, as well as the late withdrawal of the Indian summer monsoon, during positive AMO phases. These connections could be mainly caused by internal climate variability. Opposite patterns are true for the negative phase of the AMO. | Zhe HAN Feifei LUO Shuanglin LI Yongqi GAO Tore FUREVIK Lea SVENDSEN | 2016 | Advances in Atmospheric Sciences2016，33，12： | 2 |
| 7 | Description and evaluation of the bergen climate model: ARPEGE coupled with MICOM显示文摘 | T. Furevik M. Bentsen H. Drange I. K. T. Kindem N. G. Kvamst? A. Sorteberg | 2003 | Climate Dynamics2003，，1： | 1 |
| 8 | Description and evaluation of the bergen climate model: ARPEGE coupled with MICOM显示文摘 | T. Furevik M. Bentsen H. Drange I. K. T. Kindem N. G. Kvamst? A. Sorteberg | 2003 | Climate Dynamics2003，，1： | 1 |
| 9 | Demand feeding in salmon farming by hydro acoustic food detection显示文摘 | JUELL J E FUREVIK D BJORDAL A | 1993 | Aquacuhural Engineering1993，12，： | 1 |
| 10 | Description and evaluation of the bergen climate model: ARPEGE coupled with MICOM显示文摘 | T. Furevik M. Bentsen H. Drange I. K. T. Kindem N. G. Kvamst? A. Sorteberg | 2003 | Climate Dynamics2003，，1： | 1 |
| 11 | Simulated variability of the Atlantic meridional overturning circulation显示文摘 | M. Bentsen H. Drange T. Furevik T. Zhou | 2004 | Climate Dynamics (-)2004，，6： | 1 |
| 12 | Description and evaluation of the bergen climate model: ARPEGE coupled with MICOM显示文摘 | T. Furevik M. Bentsen H. Drange I. K. T. Kindem N. G. Kvamst? A. Sorteberg | 2003 | Climate Dynamics2003，，1： | 1 |
| 13 | Evaluation of treat- ment and post-treatment changes by the PAR index 显示文摘 | Birkeland K Furevik J Boe OE | 1997 | Eur J Orthod1997，19，3： | 1 |
| 14 | Enaluation of treat-ment and post-treatment changes by the PAR index显示文摘 | BIRKEAND K FUREVIK J ROE O E | 1997 | Eur J Orthod1997，19，3： | 1 |
| 15 | Nearshore wave forecasting and hindcasting by dynamical and statistical downscaling显示文摘 | Breivik R Gusdal Y Furevik B R | 2009 | Journal of Marine Systems2009，78，： | 1 |
| 16 | Distribution and abundance of fish in deep-sea coral habitats显示文摘 | HUSEBO A NφTTESTAD L FOSSA J H FUREVIK D M JORGENSEN S B | 2002 | Hydrobiologia2002，471，： | 1 |
| 17 | Description and evaluation of the bergen climate model: ARPEGE coupled with MICOM显示文摘 | T. Furevik M. Bentsen H. Drange I. K. T. Kindem N. G. Kvamst? A. Sorteberg | 2003 | Climate Dynamics2003，，1： | 1 |
| 18 | The deep-water coral Lophelia pertusa in Norwegian waters : distribution and fishery impacts 显示文摘 | FOSSA J H MORTENSEN P B FUREVIK D M | 2002 | Hydrobiologia2002，471，： | 1 |
| 19 | Demand feeding in salmon farming by hydroacoustic food detection 显示文摘 | JUELL J E FUREVIK D M BJORDAL A | 1993 | Aquacuhural Engineering1993，12，3： | 1 |
| 20 | Evaluation of treatment and post-treatment changes by the PAR Index显示文摘 | Birkeland K Furevik J Boe O E | 1997 | Eur J Orthod1997，19，3： | 1 |
您所在的机构暂未开通此部分的功能，请联系管理员