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林业科学 ›› 2025, Vol. 61 ›› Issue (2): 50-61.doi: 10.11707/j.1001-7488.LYKX20220728

• 研究论文 • 上一篇    下一篇

1960—2050年中国竹林区极端气候的时空变化

单博文1(),李祎1,覃钧1,石雷1,2,*()   

  1. 1. 国家林业和草原局/北京市共建竹藤科学与技术重点实验室 国际竹藤中心 北京 100102
    2. 滇南竹林生态系统国家定位观测研究站 沧源 677400
  • 收稿日期:2022-10-26 出版日期:2025-02-25 发布日期:2025-03-03
  • 通讯作者: 石雷 E-mail:15532212038@163.com;leishi@icbr.ac.cn
  • 基金资助:
    国际竹藤中心基本业务费专项基金(1632018010);国家重点研发计划项目(2016YFD0600902)。

Spatiotemporal Change of the Extreme Climate in China’s Bamboo Forest during 1960—2050

Bowen Shan1(),Yi Li1,Jun Qin1,Lei Shi1,2,*()   

  1. 1. Key Laboratory of National Forestry and Grassland Administration/Beijing for Bamboo & Rattan Science and Technology International Center for Bamboo and Rattan Beijing 100102
    2. National Positioning Observation and Research Station of Bamboo Forest Ecosystem in Southern Yunnan Province Cangyuan 677400
  • Received:2022-10-26 Online:2025-02-25 Published:2025-03-03
  • Contact: Lei Shi E-mail:15532212038@163.com;leishi@icbr.ac.cn

摘要:

目的: 探究中国竹林分布区极端气候的时空变化,揭示极端气候事件发生的空间分异及其时间变化规律,为未来不同竹林分布区应对极端气候事件提供参考。方法: 基于1960—2020年气象数据,利用中国天气发生器(NCC/GU-WG Version 2.0)对2021—2050年的气象数据进行预测,借助RClimDex软件计算与竹林生长相关的10个极端气候指标,采用累积距平、Sen趋势、Mann-Kendall检验和克里金插值法研究1960—2050年中国竹林分布区极端气候的时空分布及其变化规律。结果: 90年来,中国竹林区的夏季高温日数、日最高温的极高值、日最低温的极高值、日最高温的极低值和日最低温的极低值每10年分别上升3.52天、0.15 ℃、0.21 ℃、0.26 ℃和0.4 ℃,霜冻日数每10 年减少1.79天,上述极端温度指标大约在2000年前后存在突变点;单日最大降水量、连续5日最大降水量、强降水量和年均日降水强度每10年分别上升1.58 mm、2.13 mm、12.99 mm和0.2 mm?d?1,上述极端降水指标在1994年前后存在突变点。从空间上来看,日最高温和日最低温的极高值在整个竹林区域都较大,而夏季高温日数的高值区则位于低纬度的竹林区;日最高温和日最低温的极低值的低值区,以及霜冻日数的高值区主要位于内陆高纬度的散生竹区。表征极端降水的单日最大降水量、连续5日最大降水量、强降水量和年均日降水强度的高值区位于南方以及沿海区域,而四川混生竹区具有较高的极端降水指标和极低的极端低温指标。结论: 在中国竹林分布区发生的极端温度和降水事件都具有明显的增加趋势,且大部分极端温度指标和极端降水指标分别在2000年前后和1994年前后存在突变点。内陆高纬度区域的散生竹区易遭受极端低温事件的影响,低纬度竹林区可能会遭受旱涝两极灾害的影响,而四川混生竹区遭受极端温度和极端降水事件的风险均相对较高。

关键词: 散生竹, 混生竹, 丛生竹, 极端温度, 极端降水, 空间分布

Abstract:

Objective: As a special forest type in China, bamboo forest is susceptible to extreme climate. It is of great significance to examine the spatiotemporal patterns of extreme climate events in China’s bamboo forests, which can unveil the spatial differentiation and temporal change patterns and thus provide a reference to cope with extreme climate events in the future. Method: In this paper, based on the meteorological data from 1960 to 2020, we used the China Weather Generator (NCC/GU-WG Version 2.0) to forecast the meteorological data from 2021 to 2050, and calculate the commonly used 10 extreme climate indices related to bamboo growth by RClimDex software. Then accumulative anomalies, Sen trend, Mann-Kendall test, and Kriging interpolation were employed to study the spatiotemporal distribution of extreme climate and its change in China’s bamboo forests. Result: From 1960 to 2050, number of hot summer days, maximum values of daily maximum and daily minimum temperatures, minimum values of daily maximum and daily minimum temperatures increased by 3.52 d, 0.15 ℃, 0.21 ℃, 0.26 ℃ , and 0.4 ℃ every 10 years, respectively, while frost days decreased 1.79 d every 10 years, and the aforementioned extreme temperature indices had abrupt changes around 2000. Maximum daily precipitation, maximum five-day precipitation, heavy precipitation, and average annual daily precipitation intensity increased by 1.58 mm, 2.13 mm, 12.99 mm , and 0.2 mm?d?1 every 10 years, respectively, and all the extreme precipitation indices had abrupt changes around 1994. Spatially, the low-value areas of maximum value of daily maximum and daily minimum temperatures representing extreme high temperatures, and high-value areas of frost days were mainly located in the monopodial bamboo areas at high inland latitude. The minimum value of daily maximum and daily minimum temperatures representing extreme low temperatures were larger throughout the region, the high-value areas of summer days were located in bamboo forest areas at low latitudes, and the high-value areas of extreme precipitation lied in the southern and coastal regions. Conclusion: Both temperature and precipitation extremes are significantly increasing in China’s bamboo forest. Monopodial bamboo areas located in high inland latitude might be vulnerable to extreme low temperature events, while the bamboo forest at low latitudes is more likely to suffer from both drought and flood disasters, and the mixed bamboo areas of Sichuan encountering extreme temperature and precipitation events are both relatively high.

Key words: monopodial bamboo, mixed bamboo, sympodial bamboo, extreme temperature, extreme precipitation, spatial distribution

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