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  • 1
    Online Resource
    Online Resource
    Copernicus GmbH ; 2019
    In:  Atmospheric Chemistry and Physics Vol. 19, No. 13 ( 2019-07-05), p. 8563-8568
    In: Atmospheric Chemistry and Physics, Copernicus GmbH, Vol. 19, No. 13 ( 2019-07-05), p. 8563-8568
    Type of Medium: Online Resource
    ISSN: 1680-7324
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2019
    detail.hit.zdb_id: 2092549-9
    detail.hit.zdb_id: 2069847-1
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  • 2
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2017
    In:  Journal of Meteorological Research Vol. 31, No. 5 ( 2017-10), p. 820-833
    In: Journal of Meteorological Research, Springer Science and Business Media LLC, Vol. 31, No. 5 ( 2017-10), p. 820-833
    Type of Medium: Online Resource
    ISSN: 2095-6037 , 2198-0934
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2017
    detail.hit.zdb_id: 2782783-5
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  • 3
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2015
    In:  Climatic Change Vol. 129, No. 1-2 ( 2015-3), p. 197-211
    In: Climatic Change, Springer Science and Business Media LLC, Vol. 129, No. 1-2 ( 2015-3), p. 197-211
    Type of Medium: Online Resource
    ISSN: 0165-0009 , 1573-1480
    RVK:
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2015
    detail.hit.zdb_id: 751086-X
    detail.hit.zdb_id: 1477652-2
    SSG: 14
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  • 4
    In: International Journal of Climatology, Wiley, Vol. 38, No. 11 ( 2018-09), p. 4077-4091
    Abstract: The Silk Road Economic Belt and 21st‐century Maritime Silk Road is a development initiative proposed by the Chinese government. However, the Belt and Road regions involve a large population, and regional economic development is sensitive to climate change, particularly climate extreme events. Hence, it is of vital relevance to pay more attention to the climate extreme change over this region. In this study, changes in the temperature‐ and precipitation‐related extremes over the Belt and Road regions are evaluated during the middle and the end of this century using Coupled Model Intercomparison Project Phase 5 (CMIP5) simulations. Results present obvious changes in extreme temperature and precipitation indices under both RCP4.5 (representative concentration pathways) and RCP8.5 scenarios against the current climate state (1986–2005). Changes generally present relatively larger magnitudes under RCP8.5 than RCP4.5. Projected multi‐model ensemble results show a significant increase in warm events over Moscow and Nairobi. Additionally, cold events will decrease over central Europe, Moscow and central Asia, along with longer growing season length over these regions. The annual mean precipitation is reported to significantly increase over the region of Nairobi and the flooding events will be exacerbated across the Belt regions under a future warmer world, particularly over Moscow, Southeast Asia and Nairobi. Meanwhile, the region of West Asia will be likely to experience more drought and flooding events with the warming. However, we should also note that the inter‐model uncertainty of these results is reported to increase with time and a relatively large model spread can be seen in precipitation‐related indices when comparing with the temperature.
    Type of Medium: Online Resource
    ISSN: 0899-8418 , 1097-0088
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2018
    detail.hit.zdb_id: 1491204-1
    SSG: 14
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  • 5
    Online Resource
    Online Resource
    Wiley ; 2015
    In:  International Journal of Climatology Vol. 35, No. 10 ( 2015-08), p. 2735-2751
    In: International Journal of Climatology, Wiley, Vol. 35, No. 10 ( 2015-08), p. 2735-2751
    Abstract: The science that humans are the cause of global warming, and that the associated climate change would lead to serious changes in climate extreme events, food production, freshwater resources, biodiversity, human mortality, etc. is unequivocal. After several political negotiations, a 2 °C warming has been considered to be the benchmark for such damaging changes. However, an increasing amount of scientific research indicates that higher levels of warming are increasingly likely. What would the world be like if such higher levels of warming occurred? This study aims to provide information for better politically driven mitigation through an investigation of the changes in temperature‐ and precipitation‐based extreme indices using CMIP5 (coupled model intercomparison project phase 5) simulations of a warming of 1, 2, and 3 °C in China. Warming simulations show more dramatic effects in China compared with the global average. In general, the results show relatively small change signals in climate extreme events in China at 1 °C, larger anomalies at 2 °C, and stronger and more extended anomalies at 3 °C. Changes in the studied temperature indices indicate that warm events would be more frequent and stronger in the future, and that cold events would be reduced and weakened. For changes in the precipitation indices, extreme precipitation generally increases faster than total wet‐day precipitation, and China will experience more intensified extreme precipitation events. Furthermore, the risk of flooding is projected to increase, and the dry conditions over northern China are projected to be mitigated. In certain regions, particularly Southwest China, the risks of both drought and flood events would likely increase despite the decreased total precipitation in the future. Uncertainties mainly derived from inter‐model and scenario variabilities are attached to these projections, but a high model agreement can be generally observed in the likelihood of these extreme changes.
    Type of Medium: Online Resource
    ISSN: 0899-8418 , 1097-0088
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2015
    detail.hit.zdb_id: 1491204-1
    SSG: 14
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  • 6
    Online Resource
    Online Resource
    Wiley ; 2017
    In:  International Journal of Climatology Vol. 37, No. S1 ( 2017-08), p. 138-156
    In: International Journal of Climatology, Wiley, Vol. 37, No. S1 ( 2017-08), p. 138-156
    Abstract: This study aimed to characterize present and future drought changes over eastern China using observations and Coupled Model Intercomparison Project Phase 5 ( CMIP5 ) simulations. We used the standardized precipitation evapotranspiration index ( SPEI ) to characterize droughts at the timescales of 3‐ and 12‐month. We distinguished the spatial patterns of drought regimes ( DRs ) using the rotated empirical orthogonal function ( EOF ) on the SPEI . Our results identified three DRs centered in northern China ( DR1 ), northeastern China ( DR2 ), and southern China ( DR3 ). Droughts in these regimes have increased in recent decades. Most CMIP5 models reproduce at least two of the DRs. The rotated EOF results indicate that the three DRs can jointly explain 46–68% of the SPEI variance (compared with approximately 60% in the observations). Among the 33 CMIP5 models analysed in this study, 13 simulated all three DRs well and showed a strong correlation pattern ( 〉 0.5). Further analysis indicated that both the external natural and greenhouse gas forcing experiments in CMIP5 reproduced the DRs, implying that natural variability and anthropogenic activity play important roles in the formation of these DRs. With continued climate warming, the three DRs over eastern China will persist. Despite the uncertainties in drought changes that mainly depend on the potential evapotranspiration methods, climate model results suggest that droughts would be aggravated under warming scenarios. The probability of severe droughts increase by the end of the century: 33% in DR1 , 25% in DR2 , 34% in DR3 in RCP4 .5 and almost double in RCP8 .5 scenario in Thornthwaite method based SPEI estimates.
    Type of Medium: Online Resource
    ISSN: 0899-8418 , 1097-0088
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2017
    detail.hit.zdb_id: 1491204-1
    SSG: 14
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  • 7
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2017
    In:  Geophysical Research Letters Vol. 44, No. 5 ( 2017-03-16), p. 2436-2444
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 44, No. 5 ( 2017-03-16), p. 2436-2444
    Abstract: Human influences have increased daily precipitation extremes by approximately 13% over China in recent decades For 1.5°C of warming the fraction of precipitation extremes attributable to human influences increases to approximately 51% Precipitation extremes over Tibetan Plateau show the highest sensitivity to human influence
    Type of Medium: Online Resource
    ISSN: 0094-8276 , 1944-8007
    URL: Issue
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2017
    detail.hit.zdb_id: 2021599-X
    detail.hit.zdb_id: 7403-2
    SSG: 16,13
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  • 8
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2015
    In:  Journal of Geophysical Research: Atmospheres Vol. 120, No. 12 ( 2015-06-27), p. 5895-5909
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 120, No. 12 ( 2015-06-27), p. 5895-5909
    Abstract: Analysis performed on daily visibility data from 1960 to 2012 Haze primarily occurs in boreal winter and in morning in North China Haze occurrence closely linked to northward activity of East Asian jet stream
    Type of Medium: Online Resource
    ISSN: 2169-897X , 2169-8996
    URL: Issue
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2015
    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 2969341-X
    SSG: 16,13
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  • 9
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2017
    In:  Journal of Geophysical Research: Atmospheres Vol. 122, No. 13 ( 2017-07-16), p. 6899-6914
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 122, No. 13 ( 2017-07-16), p. 6899-6914
    Abstract: Extreme precipitation has clearly increased in recent decades across China The emerging signal of anthropogenic activities is detected in changes in extreme precipitation over China and is generally dominated by greenhouse gas emissions Large uncertainties still exist due to the effects of natural external forcings and anthropogenic aerosols
    Type of Medium: Online Resource
    ISSN: 2169-897X , 2169-8996
    URL: Issue
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2017
    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 2969341-X
    SSG: 16,13
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  • 10
    Online Resource
    Online Resource
    Wiley ; 2016
    In:  International Journal of Climatology Vol. 36, No. 9 ( 2016-07), p. 3226-3236
    In: International Journal of Climatology, Wiley, Vol. 36, No. 9 ( 2016-07), p. 3226-3236
    Abstract: Previous studies have documented that the summer precipitation over South China ( SC ) has experienced a prominent inter‐decadal increase in 1992/1993, and the possible mechanism has been well revealed. The aim of this study is to investigate the changes in extreme precipitation and clustered extreme precipitation events in recent decades using station observations and the National Centers for Environmental Prediction/National Center for Atmospheric Research ( NCEP / NCAR ) reanalysis data. The results indicate that extreme precipitation also experienced a significant inter‐decadal increase around 1992/1993. Significant changes can also be found in the associated atmospheric circulations, such as the western North Pacific subtropical high ( WNPSH ) and the westerly jet stream over East Asia. In addition, the water vapour transport ( WVT ) related to extreme precipitation differed from mean conditions. For extreme precipitation events, the WVT from the Northwest Pacific and Indian Oceans was much stronger when compared with mean precipitation. When extreme precipitation events were clustered, the increased WVT mainly originated from the South China Sea and Northwest Pacific Ocean. Further analysis indicates that the WVT increased from the Indian Ocean but decreased from the Northwest Pacific after 1992/1993; this finding explains the significant increase in the clustered extreme precipitation events over SC after 1992/1993. In addition, the atmospheric stratification has become more unstable since 1992/1993.
    Type of Medium: Online Resource
    ISSN: 0899-8418 , 1097-0088
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2016
    detail.hit.zdb_id: 1491204-1
    SSG: 14
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