Q4 Social Sciences
L. Chojnacka-Ożga, Wojciech Ożga
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引用次数: 0

摘要

气候监测应用和预测森林生态系统对气候变化的响应经常使用由气温得出的生长季节长度指数。森林生态系统研究中最广泛使用的指标是热生长季节的长度(温度≥5°C),较少使用森林生长季节的参数(温度≥10°C)。然而,只有少数研究使用了森林中长期的一系列温度测量。本文测定了1951-2020年华沙生命科学大学实验森林Rogów (51,040 ' n, 19o55'E, h = 194 m MSL)热(TGS)和森林(FGS)生长季节参数的时间变化。该分析基于位于森林综合体附近的气象站和位于120多年历史的新鲜混交林中的林冠下站获得的数据集(日平均气温)。结果表明:1951—2020年,生长季明显延长,TGS平均延长2.8 d /10 a, FGS平均延长2.4 d /10 a;TGS和FGS的延长是其早开始和晚结束的结果。TGS开始呈显著负向变化(1.3 d /10年),近30年变化最显著(4.4 d /10年)。过去30年的特征还表现为统计上显著的TGS后期趋势。1991-2020年的TGS比1951-1980年和1971-2000年的TGS长9天,1981-2010年的TGS长5天。TGS长度的变化主要是由于其开始时间较早:在1991-2020年的多年期,TGS开始时间比1951-1980年早7天。在FGS的情况下,这些变化较弱,尽管在统计上,FGS开始日期呈显著的负趋势,而FGS长度呈显著的正趋势。FGS比TGS晚一个月(平均4月28日),提前4周(平均10月5日)结束,持续了160天。林内TGS比林外短3 d, FGS比林外短1 d。近30年TGS开始的加速速度快于无霜期开始的速度,表明植被暴露于春霜的可能增加。这可能会对植被第一阶段的植物发育造成威胁。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Charakterystyka okresu wegetacyjnego w Lasach Doświadczalnych SGGW w Rogowie w latach 1951–2020
The growing season length indices derived from air temperature are frequently used in climate monitoring applications as well as to predict the response of forest ecosystems to climate change. The indicator most widely used in the studies of forest ecosystems is the length of the thermal growing season (temp ≥5°C), less commonly the parameters of the forest growing season (temp ≥10°C). However, only a few studies used long-term series of temperature measurements in the forest. In this article, we determined the temporal changes in the parameters of the thermal (TGS) and forest (FGS) growing season in the Experimental Forests of the Warsaw University of Life Sciences in Rogów (51o40’N, 19o55’E, h = 194 m MSL) in the years 1951–2020. The analysis is based on the dataset (daily mean air temperature) obtained from a meteorological station located near the forest complex and from a forest under-canopy station located in a more than 120-year-old fresh mixed forest. The results show a significant extension of the growing season in 1951–2020, the TGS lasted on average 2.8 days/10 years, and the FGS 2.4 days/10 years. The extension of the TGS and FGS was a consequence of both its earlier start and later end. The start of the TGS was characterized by a statistically significant negative trend (1.3 days/10 years), and most changes were characteristic for the last three decades (4.4 days/10 years). The last 30 years were also characterized by a statistically significant trend towards the later end of the TGS. The TGS in 1991–2020 was longer than in 1951–1980 and 1971–2000 by 9 days, while in 1981–2010 by 5 days. Changes in the length of the TGS resulted primarily from its earlier beginning: in the multi-year period 1991–2020, the TGS started 7 days earlier than in 1951–1980. In the case of the FGS, these changes were weaker, although there was a statistically significant negative trend in the start dates and a positive trend in the FGS length. The FGS started almost a month later than the TGS (average on April 28) and ended 4 weeks earlier (average on October 5) and lasted 160 days. TGS in the forest was shorter than outside the forest by 3 days, and FGS by 1 day. The acceleration of the beginning of TGS during the last three decades was faster than the beginning of the frost-free period, indicating a possible increase in vegetation exposure to spring frost. This may pose a threat to the development of plants in the first phase of vegetation.
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来源期刊
Prace i Studia Geograficzne
Prace i Studia Geograficzne Social Sciences-Cultural Studies
CiteScore
0.40
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0.00%
发文量
26
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