Yunxia Dong , Guimin Liu , Xiaodong Wu , Lin Wang , Sizhong Yang , Tonghua Wu , Haiyan Xu , Evgeny Abakumov , Jun Zhao , Xingyuan Cui , Meiqi Shao
{"title":"1982-2022年北方多年冻土区极端气候时空变化及其对植被生长的影响","authors":"Yunxia Dong , Guimin Liu , Xiaodong Wu , Lin Wang , Sizhong Yang , Tonghua Wu , Haiyan Xu , Evgeny Abakumov , Jun Zhao , Xingyuan Cui , Meiqi Shao","doi":"10.1016/j.catena.2025.109420","DOIUrl":null,"url":null,"abstract":"<div><div>The permafrost regions of the northern hemisphere are increasingly experiencing frequent and intense extreme climate, which may significantly impact the vegetation growth. However, the effects of extremes on vegetation are often overlooked, leading to an underestimation of their impacts on vegetation. Here we provide a comprehensive analysis of the spatiotemporal variations of extreme climate in the northern permafrost regions from 1982 to 2022, as well as the responses of vegetation growth to these changes in growing-seasons. The results show that: (1) the occurrence of warm days and nights increased, with nighttime temperature rises exceeding those during the day. The changing trend of extreme warm indices was less pronounced than that of extreme cold indices; (2) The frequency and duration of extreme precipitation had significantly increased, with slight changes in precipitation intensity; (3) The extreme temperature events largely showed no cumulative and lagged effects on vegetation growth, and the areas with one-month lag and two-month cumulative effects of extreme precipitation ranged from 19.1 % to 42.9 %; (4) The relationship between vegetation growth and extreme climate events varied by vegetation type. Grasslands, forests, and shrubs were mainly affected by the one-month lag and two-month cumulative effect of extreme precipitation, whereas wetlands exhibited a predominant one-month lag effect. Overall, our results suggested that the effects of extreme climate on vegetation growth in northern permafrost regions were mainly manifested by the cumulative and lagged effects of precipitation from 1982 to 2022, and more attentions should be paid to extreme precipitation in modelling vegetation growth under a changing climate in the permafrost regions.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":"260 ","pages":"Article 109420"},"PeriodicalIF":5.7000,"publicationDate":"2025-09-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Spatiotemporal variations of extreme climate and their effects on vegetation growth in the northern permafrost regions during 1982–2022\",\"authors\":\"Yunxia Dong , Guimin Liu , Xiaodong Wu , Lin Wang , Sizhong Yang , Tonghua Wu , Haiyan Xu , Evgeny Abakumov , Jun Zhao , Xingyuan Cui , Meiqi Shao\",\"doi\":\"10.1016/j.catena.2025.109420\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The permafrost regions of the northern hemisphere are increasingly experiencing frequent and intense extreme climate, which may significantly impact the vegetation growth. However, the effects of extremes on vegetation are often overlooked, leading to an underestimation of their impacts on vegetation. Here we provide a comprehensive analysis of the spatiotemporal variations of extreme climate in the northern permafrost regions from 1982 to 2022, as well as the responses of vegetation growth to these changes in growing-seasons. The results show that: (1) the occurrence of warm days and nights increased, with nighttime temperature rises exceeding those during the day. The changing trend of extreme warm indices was less pronounced than that of extreme cold indices; (2) The frequency and duration of extreme precipitation had significantly increased, with slight changes in precipitation intensity; (3) The extreme temperature events largely showed no cumulative and lagged effects on vegetation growth, and the areas with one-month lag and two-month cumulative effects of extreme precipitation ranged from 19.1 % to 42.9 %; (4) The relationship between vegetation growth and extreme climate events varied by vegetation type. Grasslands, forests, and shrubs were mainly affected by the one-month lag and two-month cumulative effect of extreme precipitation, whereas wetlands exhibited a predominant one-month lag effect. Overall, our results suggested that the effects of extreme climate on vegetation growth in northern permafrost regions were mainly manifested by the cumulative and lagged effects of precipitation from 1982 to 2022, and more attentions should be paid to extreme precipitation in modelling vegetation growth under a changing climate in the permafrost regions.</div></div>\",\"PeriodicalId\":9801,\"journal\":{\"name\":\"Catena\",\"volume\":\"260 \",\"pages\":\"Article 109420\"},\"PeriodicalIF\":5.7000,\"publicationDate\":\"2025-09-08\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Catena\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0341816225007222\",\"RegionNum\":1,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Catena","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0341816225007222","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Spatiotemporal variations of extreme climate and their effects on vegetation growth in the northern permafrost regions during 1982–2022
The permafrost regions of the northern hemisphere are increasingly experiencing frequent and intense extreme climate, which may significantly impact the vegetation growth. However, the effects of extremes on vegetation are often overlooked, leading to an underestimation of their impacts on vegetation. Here we provide a comprehensive analysis of the spatiotemporal variations of extreme climate in the northern permafrost regions from 1982 to 2022, as well as the responses of vegetation growth to these changes in growing-seasons. The results show that: (1) the occurrence of warm days and nights increased, with nighttime temperature rises exceeding those during the day. The changing trend of extreme warm indices was less pronounced than that of extreme cold indices; (2) The frequency and duration of extreme precipitation had significantly increased, with slight changes in precipitation intensity; (3) The extreme temperature events largely showed no cumulative and lagged effects on vegetation growth, and the areas with one-month lag and two-month cumulative effects of extreme precipitation ranged from 19.1 % to 42.9 %; (4) The relationship between vegetation growth and extreme climate events varied by vegetation type. Grasslands, forests, and shrubs were mainly affected by the one-month lag and two-month cumulative effect of extreme precipitation, whereas wetlands exhibited a predominant one-month lag effect. Overall, our results suggested that the effects of extreme climate on vegetation growth in northern permafrost regions were mainly manifested by the cumulative and lagged effects of precipitation from 1982 to 2022, and more attentions should be paid to extreme precipitation in modelling vegetation growth under a changing climate in the permafrost regions.
期刊介绍:
Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment.
Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.