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气候变暖背景下西藏中南部苹果物候期变化及其气候影响因子分析
引用本文:杜军,蒲桂娟,索朗旺堆,王挺,巴桑. 气候变暖背景下西藏中南部苹果物候期变化及其气候影响因子分析[J]. 中国农业气象, 2023, 44(3): 171-181. DOI: 10.3969/j.issn.1000-6362.2023.03.001
作者姓名:杜军  蒲桂娟  索朗旺堆  王挺  巴桑
作者单位:1.西藏高原大气环境科学研究所/西藏高原大气环境科学研究开放实验室,拉萨 850001;2.中国气象局墨脱大气水分循环综合观测野外科学试验基地,墨脱 860700
基金项目:第二次青藏高原综合科学考察研究项目(2019QZKK0106);西藏自治区科技创新基地自主研究项目(XZ2021JR0001G);中国气象科学研究院青藏高原与极地气象科学研究所开放课题(ITPP2021K03)
摘    要:利用2001-2020年西藏泽当农业气象站苹果物候期和逐日平均气温(Tm)、最高气温(Tmax)、最低气温(Tmin)、气温日较差(DTR)、相对湿度(RH)、降水量(Pr)、日照时数(S)和≥0℃积温(∑T0)等资料,采用线性回归、Pearson相关系数和逐步回归等方法,分析近20a西藏中南部苹果物候期及生长期长度的变化趋势,以及影响的主导气候因子,以期揭示西藏高原苹果物候期变化特征及其对气候变暖的响应。结果表明:2001-2020年西藏中南部苹果除可采成熟期以1.28d·a-1的速率呈提前趋势外,其它物候期平均每年推迟2.83~7.64d;果实生长发育期长度、花期长度平均每年分别缩短8.92d和5.98d,而果树全生育期长度略有延长,速率为0.65d·a-1。各物候期Tmax趋于升高,Tmin呈降低趋势,DTR显著增大;多数物候期RH、S呈显著减少趋势;Pr在可采成熟期前以增加为主,之后趋于减少。春季物候期主...

关 键 词:苹果  物候  气候因子  变化趋势  西藏
收稿时间:2022-03-25

Phenological Change and Its Climatic Impact Factors of Apple under the Background of Climate Warming in South-Central Tibet
DU Jun,PU Gui-juan,Sonamwangdoi,WANG Ting,Pasang. Phenological Change and Its Climatic Impact Factors of Apple under the Background of Climate Warming in South-Central Tibet[J]. Chinese Journal of Agrometeorology, 2023, 44(3): 171-181. DOI: 10.3969/j.issn.1000-6362.2023.03.001
Authors:DU Jun  PU Gui-juan  Sonamwangdoi  WANG Ting  Pasang
Affiliation:1.Tibet Institute of Plateau Atmospheric and Environmental Science Research/Tibet Open laboratory of Plateau Atmospheric and Environmental Science Research, Lhasa 850001, China; 2.Field Science Experiment Base for Comprehensive Observation of Atmospheric Water Cycle in Mêdog County, CMA, Mêdog 860700
Abstract:To reveal the characteristics of apple phenology changes and its response to climate warming on the Tibetan plateau, with a view to providing basic scientific and technological support for local apple cultivation, management, breeding and coping with climate change. Both phenological data and meteorological items measured in the period of apple growth in Tsedang agrometeorological station from 2001 to 2020 were analyzed, which include phenological dates and the daily mean value of several meteorological factors such as mean temperature(Tm), maximum temperature(Tmax), minimum temperature(Tmin), diurnal temperature range(DTR), precipitation(Pr), relative humidity(RH), sunshine duration(S), and accumulated temperature above 0℃(∑T0) et al. Statistical methods, including linear regression, Pearson correlation coefficient and stepwise regression, were used to reveal the trends and identify the leading factors caused the changes in apple phenology in south-central Tibet in the past 20 years. The results indicated that: (1) all of the apple phenological dates were postponed in a range from 2.83 to 7.64d·y−1 in south-central Tibet from 2001 to 2020 except for the fruit maturing date (FMD), which exhibited an advanced rate of 1.28d·y−1. The length of fruit growing period (LFG) and flowering duration (FD) were shortened by 8.92d·y−1 and 5.98d·y−1, respectively, while the length of tree growing season(LTG) was slightly extended at an increasing rate of 0.65d·y−1. These results were different from the main apple producing areas in northern China where the autumn phenophase was delayed and the spring phenophase was advanced, and may be attributed to the reduction of ∑T0 during the growth seasons. (2) For all of apple phenological stages, the Tmax has increased with Tmin decreasing, leading to a significant larger value of DTR. For most of the phenological stages, RH and S have reduced significantly, while Pr increased before FMD and decreased afterwards. (3) In spring, temperature was identified as the dominant factor with negative correlation with the phenophase in south-central Tibet. In contrast, Pr was the leading factor causing changes in autumn phenophases, which was positively correlated with the FMD and negatively correlated with both the end of leaf coloring date (LCD) and the end of leaf fall date (LFD). (4) For most of the phenology, ∑T0 has been revealed as the leading factor influencing the length of phenological period. However, Tm has played the dominant roles influencing the length of the whole period and the period from the FMD to LCD, and S can be viewed as the leading factor influencing the length of the period from the LCD to LFD. It has been identified that the first flowering date was advanced by 2.32 days when Tmax increased by 1°C in early March, and the LFD was advanced by 8.55 days when Pr changed with 10mm in late October in this study region.
Keywords:Malus pumila  Phenology  Climatic factor  Change trend  Tibet  
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