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  • Xu, Huiwen  (5)
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  • 1
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2022
    In:  Earth's Future Vol. 10, No. 2 ( 2022-02)
    In: Earth's Future, American Geophysical Union (AGU), Vol. 10, No. 2 ( 2022-02)
    Abstract: Anthropogenic influence, dominated by greenhouse gas emissions, is detectable in intensified precipitation extremes over China Anthropogenic aerosols may partially offset the role of greenhouse gases in the observed increases The observation‐constrained projections show smaller increases for precipitation extremes than the raw CMIP6 outputs
    Type of Medium: Online Resource
    ISSN: 2328-4277 , 2328-4277
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2022
    detail.hit.zdb_id: 2746403-9
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  • 2
    Online Resource
    Online Resource
    Wiley ; 2022
    In:  International Journal of Climatology Vol. 42, No. 1 ( 2022-01), p. 635-651
    In: International Journal of Climatology, Wiley, Vol. 42, No. 1 ( 2022-01), p. 635-651
    Abstract: A comparison assessment of model capabilities in simulating precipitation extremes across China was first implemented by using 30 models from the Coupled Model Intercomparison Project Phase 5 (CMIP5) and using 36 CMIP6 models. The results indicate that the multi‐model median ensembles (MME) of both the CMIP5 and CMIP6 models can reasonably reproduce the climate means for the period from 1986 to 2005, and the biases are lower in most CMIP6 models compared to the CMIP5 models, especially over southern China. To provide further comparisons, 14 CMIP6 models are selected and compared with their predecessors in CMIP5. The results show that the CMIP6 models generally exhibit superior skill in simulating the extreme precipitation indices over China. The model spreads for most of the extreme indices in the CMIP6 version are also smaller. Additionally, the MMEs of the two CMIPs outperform individual models. However, some CMIP6 models also exhibit weaker skill levels in simulating some particular indices compared with those in CMIP5, which merits further investigation. The results from seven reanalyses further show large uncertainties for these indices; therefore, care should be taken in comparison with reanalyses. For future changes in precipitation extremes, total wet day precipitation (PRCPTOT), maximum 5‐day precipitation (RX5day) and very heavy precipitation days (R20mm) are projected to clearly increase across China over the coming century under the shared socioeconomic pathway (SSP) 2‐4.5 and SSP5‐8.5 scenarios. However, the dry condition index of CDD exhibits a decreasing tendency in the future, which implies that the dry conditions induced by precipitation anomalies will be mitigated. However, large uncertainties are still observed for future changes, which are primarily sourced from inter‐model and scenario variabilities, especially for the projected changes at the end of the 21st century.
    Type of Medium: Online Resource
    ISSN: 0899-8418 , 1097-0088
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2022
    detail.hit.zdb_id: 1491204-1
    SSG: 14
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  • 3
    Online Resource
    Online Resource
    Wiley ; 2021
    In:  International Journal of Climatology Vol. 41, No. 6 ( 2021-05), p. 3425-3438
    In: International Journal of Climatology, Wiley, Vol. 41, No. 6 ( 2021-05), p. 3425-3438
    Abstract: This study explores the spatial–temporal variations in summer extreme precipitation over Southwestern China (SWC). The frequency of summer extreme precipitation (FEP) has exhibited strong interannual variation with slightly strengthened intensity in recent decades. The associated anomalous water vapour transport mainly originates from northern China, the Indian Ocean, the South China Sea and the Northwest Pacific. The high FEP over SWC is generally associated with the strong Eurasian (EU) pattern and the pattern that is similar to Pacific‐Japan (PJ) teleconnection. The results further indicate that the anomalous May Arctic sea ice concentration and the sea surface temperature anomaly over the Northwest Pacific play an important role in the variation of FEP over SWC. On the one hand, the reduction in Arctic sea ice concentration intensifies Rossby wave propagation and then stimulates the formation of EU teleconnection pattern. The associated anomalous northeasterly integrated water vapour transport and high‐level westerly anomalies can result in strong interannual changes in FEP over SWC. On the other hand, the sea surface temperature anomaly over the Northwest Pacific can induce an anomalous PJ‐like pattern, and the associated anomalous southwesterly water vapour transport also exerts an impact on the change in FEP over SWC.
    Type of Medium: Online Resource
    ISSN: 0899-8418 , 1097-0088
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2021
    detail.hit.zdb_id: 1491204-1
    SSG: 14
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  • 4
    Online Resource
    Online Resource
    Elsevier BV ; 2020
    In:  Science Bulletin Vol. 65, No. 17 ( 2020-09), p. 1415-1418
    In: Science Bulletin, Elsevier BV, Vol. 65, No. 17 ( 2020-09), p. 1415-1418
    Type of Medium: Online Resource
    ISSN: 2095-9273
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2020
    detail.hit.zdb_id: 2069521-4
    detail.hit.zdb_id: 2816140-3
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  • 5
    Online Resource
    Online Resource
    Frontiers Media SA ; 2022
    In:  Frontiers in Earth Science Vol. 10 ( 2022-8-10)
    In: Frontiers in Earth Science, Frontiers Media SA, Vol. 10 ( 2022-8-10)
    Abstract: This study investigates the future changes in dangerous precipitation extremes with multiyear return periods and the population exposure across China at the 1.5–4°C warming levels via the latest simulations from the Coupled Model Intercomparison Project Phase 6 (CMIP6). The results show that the simulations project more frequent dangerous precipitation extremes across China under the warmer climate regardless of the shared socioeconomic pathway (SSP), with more substantial occurrence increases at the high warming levels. Consequently, the population exposure to dangerous precipitation extremes is anticipated to increase persistently in most regions of China except for some parts of northwestern China and the Tibetan Plateau. For the events estimated to occur once every 10 years, the 1.5, 2.0, 3.0, and 4.0°C warming relative to the current state will result in approximately 29.9, 47.8, 72.9, and 84.3% increases in the aggregated population exposure over China under the SSP5-8.5 scenario, respectively. However, the exposure change is somewhat subject to the emission scenarios, with larger proportional increases under the regional-rivalry scenario of SSP3-7.0 compared to the fossil-fueled development scenario of SSP5-8.5. The increased exposure under all the scenarios is primarily attributed to the climate change factor, and the population change and their interaction component make a minor contribution. Furthermore, compared to the 2.0°C warmer climate, the 0.5°C less warming under the 1.5°C climate can trigger remarkable decreases of 16.5–20.8% for exposure to once-in-decade events over China. Additionally, the changes in the occurrence and exposure are much larger for the rarer events. Hence, our analyses indicate that limiting warming to 1.5°C is beneficial to reducing the impacts associated with precipitation extremes across China, particularly for the more extreme events.
    Type of Medium: Online Resource
    ISSN: 2296-6463
    Language: Unknown
    Publisher: Frontiers Media SA
    Publication Date: 2022
    detail.hit.zdb_id: 2741235-0
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