摘要
基于区域气候模式COSMO-CLM(CCLM)模拟的1960—2100年逐日最低气温数据及2000年中国土地利用数据,采用强度-面积-持续时间(Intensity-Area-Duration,IAD)方法,以全球升温1.5℃(RCP 2.6情景)和2.0℃(RCP 4.5情景)为目标,研究不同持续时间中国极端低温事件变化特征、最强极端低温事件强度与面积关系和最强中心空间分布,分析极端低温事件下耕地面积暴露度的变化规律。研究发现:(1)全球升温1.5℃情景下,持续1至9 d的极端低温事件频次相对于基准期(1986—2005年)下降30%—54%,强度变化-1%—8.8%,影响面积下降7%—21%;升温2.0℃,频次下降48%—80%,强度上升6%—11.5%,影响面积则在-14%—19%变化。(2)全球不同升温情景有可能发生强度和面积超过基准期最强事件的极端低温。全球升温1.5—2.0℃时,同等面积上的最强极端低温事件强度明显下降,但最强极端低温事件中心由西北和西南转移到华中和华南等地。(3)不同升温情景下,暴露于极端低温事件的中国耕地面积明显少于基准期,且升温幅度越高下降程度越大。最强极端低温事件的耕地暴露度则随温度的升高而增大。升温1.5℃时,华东、华北与华中等地暴露在最强极端低温事件的耕地面积相对于基准期有所增大,升温2.0℃时,华东与华北等地有大幅度上升。全球不同升温情景下,极端低温事件频次与影响面积持续下降,但强度上升;随着升温幅度的增大,这种差异变化特征越来越明显;特别应注意的是,随着温度上升,发生强度和面积超过当前记录到的最强极端低温事件的可能性增大;应加强极端事件的预警、预报和监测,减缓经济社会的损失。
Based on daily minimum temperatures simulated by the COSMO-CLM （CCLM） for 1960 - 2100 and the landuse data in 2000 in China, the Intensity-Area-Duration （IAD） method was applied to characterize the extreme low-temperature events, the relationship between the intensity and spatial coverage of extreme low-temperature events, the spatial distribution of the most severe low-temperature events, and the exposure of farmlands to extreme low-temperature events under the global war- ming of 1.5℃ （RCP 2.6 scenario） and 2.0℃ （RCP 4.5 scenario）. The results are as follows. （1） During the period of 1.5℃ warming, the frequency of extreme low-temperature events that can last for one to nine days will decrease by 30% - 54%, the intensity will change by -1% -8.8%, and the area influenced by the extreme low-temperature events will decrease by 7% - 21% compared to that during the reference period （1986 - 2005）. For the 2.0℃ warming period, the frequency of the extreme low-temperature events will decrease by 48% - 80%, the intensity will increase by 6% - 11.5%, and the area affected by ex- treme low-temperature events will change by - 14% - 19%. （2） There are possibilities that both the intensity of and the area affected by the extreme low-temperature events in the future will exceed that of the most severe event in the reference period. Intensity of the most severe event in the context of 1.5℃ warming will be stronger than that in the context of 2.0℃ warming over the same area, but the center of the most severe event might move from Northwest and Southwest China to Central and South China. （3） Farmland exposure to the extreme low-temperature events will decrease in the warming periods than in the reference period, and the higher the temperature increase, the greater the decrease. However, farmland exposure to the most severe events will increase to a certain extent in East, North and Central China in the context of 1.5℃ warming, and such in- creases are even more obvious in East and North China in the context of 2.0℃ warming. Aforementioned findings indicate that frequency and coverage of the extreme low temperature events will decrease, but their intensity might increase with the rising of temperature. With the increasing occurrence probability of the most severe event with higher intensity over larger area than that in the past, improvement of early warning is still imperative for mitigation of the societal and economic impact of extreme e vents.
出处
《气象学报》
CAS
CSCD
北大核心
2017年第3期415-428,共14页
Acta Meteorologica Sinica
基金
国家自然科学基金项目(41671211,41401056)
国家自然科学基金会和巴基斯坦科学基金会合作研究项目(41661144027)
新疆维吾尔自治区高层次引进人才项目(Y642091,Y644131)
