张鑫, 楼俊伟, 范瑜越, 王进, 贾超, 高宇, 李杏. 不同气候背景下北疆霜期的时空变化特征[J]. 沙漠与绿洲气象, 2023, 17(6): 89-95.
引用本文: 张鑫, 楼俊伟, 范瑜越, 王进, 贾超, 高宇, 李杏. 不同气候背景下北疆霜期的时空变化特征[J]. 沙漠与绿洲气象, 2023, 17(6): 89-95.
ZHANG Xin, LOU Junwei, FAN Yuyue, WANG Jin, JIA Chao, GAO Yu, LI Xing. Spatial and Temporal Variation Characteristics of Frost Period in Northern Xinjiang under Different Climatic Background[J]. Desert and Oasis Meteorology, 2023, 17(6): 89-95.
Citation: ZHANG Xin, LOU Junwei, FAN Yuyue, WANG Jin, JIA Chao, GAO Yu, LI Xing. Spatial and Temporal Variation Characteristics of Frost Period in Northern Xinjiang under Different Climatic Background[J]. Desert and Oasis Meteorology, 2023, 17(6): 89-95.

不同气候背景下北疆霜期的时空变化特征

Spatial and Temporal Variation Characteristics of Frost Period in Northern Xinjiang under Different Climatic Background

  • 摘要: 利用1961—2021年逐日最低气温、大气环流指数资料,基于常规气象统计方法,对不同气候背景下北疆地区初、终霜日和霜期的变化特征进行分析,揭示其变化规律及影响因素。结果表明:(1)初霜日在背景Ⅰ(1961—1990年)下呈较快推迟趋势,速率达0.36 d/a,背景Ⅱ(1991—2021年)下变化趋势很小;终霜日在背景Ⅰ下反呈推迟趋势,速率达0.15 d/a,在背景Ⅱ下呈较快提前趋势,速率达0.28 d/a;霜期在背景Ⅰ、Ⅱ下均呈缩短趋势,缩短速率分别为0.24、0.35 d/a。(2)在气候背景Ⅰ下霜期的缩短主要由初霜日推迟而导致,在气候背景Ⅱ下霜期的缩短主要由终霜日提前所导致。(3)北疆地区平均初霜日在背景Ⅱ下变化趋势很小是因为此时段下北疆初霜日西部提前、东部推迟,且推迟与提前的变化趋势相差较小;平均终霜日在背景Ⅰ下反呈推迟趋势的气候条件是此时段下北疆春季气温变化趋势为-0.357℃/10 a,空间变化上则是因为此时段下北疆终霜日整体呈推迟趋势,仅阿勒泰地区东部、哈密地区东部呈提前趋势,且推迟速率较大,提前速率较小。(4)由气候背景Ⅰ转为背景Ⅱ,北疆初霜日等级出现由低向高转变的趋势,终霜日和霜期则与其相反。(5)相关季节北大西洋涛动指数对于北疆地区初、终霜日的影响较显著,初霜日与夏季北大西洋涛动指数呈显著负相关,终霜日与秋季北大西洋涛动指数呈显著正相关。

     

    Abstract: Using the daily minimum temperature data from 1961 to 2021 provided by Xinjiang Meteorological Information Center and atmospheric circulation index data,based on the conventional meteorological statistical methods,the variation characteristics of the first frost day,the last frost day and the frost period in northern Xinjiang under the different climatic background were analyzed to reveal its changing rule and influencing factors.Results showed that:(1) The first frost date was delayed rapidly with a rate of 0.36 d/a under background Ⅰ,but had small change under background Ⅱ.In contrast,the last frost date was delayed with a rate of 0.15 d/a under background Ⅰ and advance with a rate of 0.28 d/a under background Ⅱ.The frost period was shortened under background Ⅰ and Ⅱ,and the shortening rates are 0.24 d/a and 0.35 d/a,respectively.(2) Under climatic background I,the shortening of frost period is mainly caused by the delay of the first frost date,while under climatic background Ⅱ,the shortening of frost period is mainly caused by the advance of the last frost date.(3) The change trend of the average first frost day in northern Xinjiang is very small under the background Ⅱ because the first frost day is advancing in the west and delaying in the east of northern Xinjiang under this background,and the change trend difference between the delaying and advancing is small;The climate condition background of the average last frost date in the climate background Ⅰ is that the spring air temperature change trend in northern Xinjiang is-0.357 ℃/10 a under this background,and the spatial variation is because the last frost date in northern Xinjiang is delayed as a whole under this background,only the eastern Altay region and the eastern Hami region show an advance trend,and the delay rate is larger,and the advance rate is smaller.(4) From climatic background I to Ⅱ,the grades of the first frost days in northern Xinjiang tended to move from low to high,while the last frost days and frost periods are the opposite.(5) The seasonal North Atlantic oscillation index has a significant effect on the first and last frost days in northern Xinjiang.The first frost days have a significant negative correlation with the summer North Atlantic oscillation index,and the last frost days have a significant positive correlation with the autumn North Atlantic oscillation index.

     

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