Page 100 - 《高原气象》2025年第5期
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             Gampe D, Zscheischler J, Reichstein M, et al, 2021. Increasing im‐  [J]. Weather and Climate Extremes, 40: 100572. DOI: 10. 1016/
                 pact  of  warm  droughts  on  northern  ecosystem  productivity  over   j. wace. 2023. 100572.
                 recent  decades[J]. Nature  Climate  Change,  11(9):  772-779.  Liu J D, Qi J L, Yin P, et al, 2024. Rising cause-specific mortality
                 DOI: 10. 1038/s41558-021-01112-8.                 risk and burden of compound heatwaves amid climate change[J].
             Eyring V, Bony S, Meehl G A, et al, 2016. Overview of the Coupled   Nature  Climate  Change,  14(11):  1201-1209. DOI:  10. 1038/
                 Model  Intercomparison  Project  Phase  6 (CMIP6)  experimental   s41558-024-02137-5.
                 design and organization[J]. Geoscientific Model Development, 9  Lu  G  M,  Li  Q  Q,  Sun  X  T,  et  al,  2024. Comparative  analysis  of
                (5): 1937-1958. DOI: 10. 5194/gmd-9-1937-2016.     peak-summer  heatwaves  in  the  Yangtze-Huaihe  River  Basin  of
             Ge F, Zhu S P, Luo H L, et al, 2021. Future changes in precipitation   China in 2022 and 2013: Thermal effects of the Tibetan Plateau
                 extremes over Southeast Asia: insights from CMIP6 multi-model   [J]. Atmospheric Research, 300: 107222. DOI:  10. 1016/j. at‐
                 ensemble[J]. Environmental Research Letters, 16(2): 024013.  mosres. 2024. 107222.
                 DOI: 10. 1088/1748-9326/abd7ad.                Lun Y R, Liu L, Cheng L, et al, 2021. Assessment of GCMs simula‐
             Guo J H, Wang X Q, Fan Y R, et al, 2023. How extreme events in   tion  performance  for  precipitation  and  temperature  from  CMIP5
                 China would be affected by global warming—insights from a bias-  to  CMIP6  over  the  Tibetan  Plateau[J]. International  Journal  of
                 corrected  CMIP6  ensemble[J]. Earth’s  Future,  11(4) :   Climatology, 41(7): 3994-4018. DOI: 10. 1002/joc. 7055.
                 e2022EF003347. DOI: 10. 1029/2022EF003347.     Luo M, Lau N C, Liu Z, 2022. Different mechanisms for daytime,
             Hao Z C, 2022. Compound events and associated impacts in China[J].  nighttime,  and  compound  heatwaves  in  southern  China[J].
                 Science, 25(8): 104689. DOI: 10. 1016/j. isci. 2022. 104689.  Weather  and  Climate  Extremes,  36:  100449. DOI:  10. 1016/j.
             He C, Kim H, Hashizume M, et al, 2022. The effects of night-time   wace. 2022. 100449.
                 warming on mortality burden under future climate change scenari‐  Merrifield A L, Simpson I R, McKinnon K A, et al, 2019. Local and
                 os: a modelling study[J]. The Lancet Planetary Health, 6(8):   nonlocal land surface influence in European heatwave initial con‐
                 e648-e657. DOI: 10. 1016/S2542-5196(22)00139-5.   dition  ensembles[J]. Geophysical  Research  Letters,  46(23):
             Hersbach H, Bell B, Berrisford P, et al, 2020. The ERA5 global re‐  14082-14092. DOI: 10. 1029/2019GL083945.
                 analysis[J]. Quarterly Journal of the Royal Meteorological Soci‐  Qin Y Q, Ma H Y, Chen H S, 2024. Comparative analysis of the spa‐
                 ety, 146(730): 1999-2049. DOI: 10. 1002/qj. 3803.  tiotemporal  patterns  and  trends  of  three  types  of  summer  heat‐
             Huang X M, Zhang T T, Jiang X W, et al, 2021. Interannual variabil‐  waves  in  China (1981-2020)  using  a  biometeorological  index
                 ity  of  mid-summer  heat  wave  frequency  over  the  Sichuan  Basin  [J]. International Journal of Climatology, 44(13): 4649-4663.
                [J]. International Journal of Climatology, 41(10): 5036-5050.  DOI: 10. 1002/joc. 8601.
                 DOI: 10. 1002/joc. 7115.                       Qiu J, 2008. China: the third pole[J]. Nature, 454(7203): 393-396.
             Jin Z R, Xu K, Ge F, et al, 2024. Boost to early spring compound   DOI: 10. 1038/454393a.
                 heatwaves over South Asia from anomalous Tibetan Plateau atmo‐  Shen C M, Zhu W, Tang X R, et al, 2024. Risk assessment and resil‐
                 spheric  heat  source[J]. Atmospheric  Research,  305:  107449.  ience enhancement strategies for urban power supply-demand im‐
                 DOI: 10. 1016/j. atmosres. 2024. 107449.          balance affected by extreme weather: a case study of Beijing[J].
             Khadka  D,  Babel  M  S, Abatan A A,  et  al,  2022. An  evaluation  of   International Journal of Disaster Risk Reduction, 106: 104471.
                 CMIP5 and CMIP6 climate models in simulating summer rainfall   DOI: 10. 1016/j. ijdrr. 2024. 104471.
                 in the Southeast Asian monsoon domain[J]. International Journal   Son J H, Seo K H, Wang B, 2020. How does the Tibetan Plateau dy‐
                 of Climatology, 42(2): 1181-1202. DOI: 10. 1002/joc. 7296.  namically  affect  downstream  monsoon  precipitation?[J]. Geo‐
             Kim M K, Yu D G, Oh J S, et al, 2020. Performance evaluation of   physical Research Letters, 47(23): e2020GL090543. DOI: 10.
                 CMIP5 and CMIP6 models on heatwaves in Korea and associated   1029/2020GL090543.
                 teleconnection patterns[J]. Journal of Geophysical Research: At‐  Sun X R, Ge F, Chen Q L, et al, 2023. How striking is the intergen‐
                 mospheres,  125 (23) :  e2020JD032583. DOI:  10. 1029/  erational  difference  in  exposure  to  compound  heatwaves  over
                 2020JD032583.                                     Southeast  Asia?[J]. Earth's  Future,  11(6):  e2022EF003179.
             Li Y, Ding Y H, Liu Y X, 2021. Mechanisms for regional compound   DOI: 10. 1029/2022EF003179.
                 hot extremes in the mid-lower reaches of the Yangtze River[J].  Tan Z Y, Liu Y Z, Shao T B, et al, 2023. Association between Tibet‐
                 International Journal of Climatology, 41(2): 1292-1304. DOI:   an  Heat  Sources  and  Heat  Waves  in  China[J]. Journal  of  Cli‐
                 10. 1002/joc. 6808.                               mate, 36(22): 7905-7924. DOI: 10. 1175/JCLI-D-22-0568. 1.
             Ling S N, Lu R Y, Liu H, et al, 2023. Interannual meridional dis‐  Vaidyanathan  A,  Kegler  S  R,  Saha  S  S,  et  al,  2016. A  statistical
                 placement  of  the  upper-tropospheric  westerly  jet  over  Western   framework to evaluate extreme weather definitions from a health
                 East Asia in Summer[J]. Advances in Atmospheric Sciences, 40  perspective:  a  demonstration  based  on  extreme  heat  events[J].
                (7): 1298-1308. DOI: 10. 1007/s00376-022-2279-8.   Bulletin of the American Meteorological Society, 97(10): 1817-
             Liu B Q, Zhu C W, Ma S M, et al, 2023. Subseasonal processes of   1830. DOI: 10. 1175/BAMS-D-15-00181. 1.
                 triple  extreme  heatwaves  over  the Yangtze  River Valley  in  2022  Wang J, Chen Y, Tett S F B, et al, 2020. Anthropogenically-driven
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