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胡桃, 吕世华, 常燕, 等, 2022. CMIP6模式对青藏高原多年冻土变 Y, et al, 2023. Progress of the impact of the Qinghai-Xizang Pla‐
化的分析预估[J]. 高原气象 . 41(2): 363-375. DOI: 10. 7522/ teau heat sources on climate anomalies in drylands of China[J].
j. issn. 1000-0534. 2022. 00009. Hu T, Lǚ S H, Chang Y, et al, Plateau Meteorology, 42(2): 257-271. DOI: 10. 7522/j. issn.
2022. Analysis and prediction of permafrost changes in Qinghai- 1000-0534. 2022. 00070.
Xizang Plateau by CMIP6 climate models[J]. Plateau Meteorolo‐ 孙亦, 王婷, 2022. 四川省极端危害性高温变化特征分析[J]. 高原
gy, 41(2): 363-375. DOI: 10. 7522/j. issn. 1000-0534. 2022. 山地气象研究, 42(2): 96-103. DOI: 10. 3969/j. issn. 1674-
00009. 2184. 2022. 02. 014. Sun Y, Wang T, 2022. Variation impact of
黄子立, 吴小飞, 毛江玉, 2021. CMIP6 模式水平分辨率对模拟我 extreme hazardous high temperature in Sichuan[J]. Plateau and
国西南地区夏季极端降水的影响评估[J]. 高原气象, 40(6): Mountain Meteorology Research, 42(2): 96-103. DOI: 10.
1470-1483. DOI: 10. 7522/j. issn. 1000-0534. 2021. zk010. 3969/j. issn. 1674-2184. 2022. 02. 014.
Huang Z L, Wu X F, Mao J Y, 2021. An evaluation for impacts 孙昭萱, 张强, 孙蕊, 等, 2022. 2022年西南地区极端高温干旱特征
of the horizontal resolution of CMIP6 models on simulating ex‐ 及其主要影响[J]. 干旱气象, 40(5): 764-770. DOI: 10. 11755/
treme summer rainfall over Southwest China[J]. Plateau Meteo‐ j. issn. 1006-7639(2022)-05-0764. Sun Z X, Zhang Q, Sun R,
rology, 40(6): 1470-1483. DOI: 10. 7522/j. issn. 1000-0534. et al, 2022. Characteristics of the extreme high temperature and
2021. zk010. drought and their main impacts in southwestern China of 2022
贾佳, 胡泽勇, 2017. 中国不同等级高温热浪的时空分布特征及趋 [J]. Arid Meteorology, 40(5): 764-770. DOI: 10. 11755/j. issn.
势[J]. 地球科学进展, 32(5): 546-559. DOI: 10. 11867/j. issn. 1006-7639(2022)-05-0764.
1001-8166. 2017. 05. 0546. Jia J, Hu Z Y, 2017. Spatial and 王丹云, 曾晓东, 宋翔, 2024. CMIP6 模式关于中国叶面积指数对
temporal features and trend of different level heat waves over Chi‐ 温度和降水变化敏感性的模拟能力评估[J]. 大气科学, 48
na[J]. Advances in Earth Science, 32(5): 546-559. DOI: 10. (5): 1-17. DOI: 10. 3878/j. issn. 1006-9895. 2304. 22067.
11867/j. issn. 1001-8166. 2017. 05. 0546. Wang D Y, Zeng X D, Song X, 2024. Evaluation of CMIP6
赖欣, 范广洲, 华维, 等, 2021. 青藏高原陆气相互作用对东亚区域 Models in simulating the sensitivity of leaf area index to tempera‐
气候影响的研究进展[J]. 高原气象, 40(6): 1263-1277. DOI: ture and precipitation changes over China[J]. Chinese Journal of
10. 7522/j. issn. 1000-0534. 2021. zk018. Lai X, Fan G Z, Hua Atmospheric Sciences, 48(5): 1-17. DOI: 10. 3878/j. issn.
W, et al, 2021. Progress in the study of influence of the Qinghai- 1006-9895. 2304. 22067.
Xizang Plateau land atmosphere interaction on East Asia Regional 王美蓉, 周顺武, 孙阳, 等, 2022. CMIP6全球气候模式对青藏高原
Climate[J]. Plateau Meteorology, 40(6): 1263-1277. DOI: 10. 中东部地表感热通量模拟能力评估[J]. 大气科学, 46(5):
7522/j. issn. 1000-0534. 2021. zk018. 1225-1238. DOI: 10. 3878/j. issn. 1006-9895. 2204. 21169.
李双双, 胡佳岚, 何锦屏, 等, 2023. 1970-2020 年秦岭南北夏季昼 Wang M R, Zhou S W, Sun Y, et al, 2022. Assessment of the
夜复合高温时空变化及其影响因素[J]. 地理研究, 42(5): Spring sensible heat flux over the central and eastern Tibetan Pla‐
1410-1424. DOI: 10. 11821/dlyj020220690. Li S S, Hu J L, He teau simulated by CMIP6 multi-models[J]. Chinese Journal of At‐
J P, et al, 2023. Variation of summertime compound hot ex‐ mospheric Sciences, 46(5): 1225-1238. DOI: 10. 3878/j. issn.
tremes over the north and south of Qinling Mountains and its in‐ 1006-9895. 2204. 21169.
fluencing factors during 1970-2020[J]. Geographical Research, 吴国雄, 刘屹岷, 何编, 等, 2018. 青藏高原感热气泵影响亚洲夏季
42(5): 1410-1424. DOI: 10. 11821/dlyj020220690. 风的机制[J]. 大气科学, 42(3): 488-504. DOI: 10. 3878/j.
李永华, 卢楚翰, 徐海明, 等, 2011. 夏季青藏高原大气热源与西南 issn. 1006-9895. 1801. 17279. Wu G X, Liu Y M, He B, et al,
地区东部旱涝的关系[J]. 大气科学, 35(3): 422-434. DOI: 2018. Review of the impact of the Tibetan Plateau sensible heat
10. 3878/j. issn. 1006-9895. 2011. 03. 04. Li Y H, Lu C H, Xu H driven air-pump on the Asian summer monsoon[J]. Chinese Jour‐
M, et al, 2011. Contemporaneous relationships between summer nal of Atmospheric Sciences, 42(3): 488-504. DOI: 10. 3878/j.
atmospheric heat source over the Tibetan Plateau and drought/ issn. 1006-9895. 1801. 17279.
flood in Eastern Southwest China[J]. Chinese Journal of Atmo‐ 吴佳, 高学杰, 2013. 一套格点化的中国区域逐日观测资料及与其
spheric Sciences, 35(3): 422-434. DOI: 10. 3878/j. issn. 1006- 它资料的对比[J]. 地球物理学报, 56(4): 1102-1111. DOI:
9895. 2011. 03. 04. 10. 6038g20130406. Wu J, Gao X J, 2013. A gridded daily obser‐
刘晓冉, 程炳岩, 杨茜, 等, 2009. 川渝地区夏季高温干旱变化特征 vation dataset over China region and comparison with the other
及其异常年环流形势分析[J]. 高原气象, 28(2): 306-313. Liu datasets[J]. Chinese Journal of Geophysics, 56(4): 1102-1111.
X R, Cheng B Y, Yang Q, et al, 2009. Changing characteristics DOI: 10. 6038g20130406.
of high temperature and drought of Sichuan-Chongqing Regions 杨崧, 徐连连, 2024. 泛南海地区极端降水的历史分布和未来演变
in summer and its analysis of circulation patterns in anomalous 特征[J]. 大气科学, 48(1): 333-346. DOI: 10. 3878/j. issn.
years[J]. Plateau Meteorology, 28(2): 306-313. 1006-9895. 2307. 23308. Yang S, XU L L, 2024. Extreme pre‐
罗红羽, 于海鹏, 胡泽勇, 等, 2023. 青藏高原热源对我国旱区气候 cipitation in the South China Sea and surrounding areas: observa‐
异常影响研究进展[J]. 高原气象, 42(2): 257-271. DOI: 10. tion and projection[J]. Chinese Journal of Atmospheric Sciences,
7522/j. issn. 1000-0534. 2022. 00070. Luo H Y, Yu H P, Hu Z 48(1): 333-346. DOI: 10. 3878/j. issn. 1006-9895. 2307. 23308.

