Xuanwei He , Xiangyang Liu , Jing Li , Yitao Li , Wenping Yu , Zhao-Liang Li
{"title":"2006 - 2019年中纬度北部生物物理温度响应实际土地覆盖变化的时间趋势","authors":"Xuanwei He , Xiangyang Liu , Jing Li , Yitao Li , Wenping Yu , Zhao-Liang Li","doi":"10.1016/j.agrformet.2025.110667","DOIUrl":null,"url":null,"abstract":"<div><div>The biophysical effects of land cover change (LCC) on land surface temperature (LST) have garnered increasing attention. However, previous studies mainly focused on their spatial patterns, leaving temporal trends relatively underexplored. In this study, we selected the densely populated northern mid-latitudes region (NM, 20°N-50°N) as study area, and analyzed the temporal trends in biophysical temperature effects of LCC using long-term satellite observations. The key findings are as follows: (1) from 2006 to 2019, five dominant types of LCC were identified in the NM region, including conversion from barren land to grassland, grassland to barren land, cropland loss, urbanization, and cropland expansion; (2) although the net temperature effect of all LCCs during the study period was relatively small (0.003 K with a declining trend of -0.012 K/decade), this reflected the offsetting impacts of different LCC types, highlighting the importance of analyzing their distinct biophysical effects; (3) urbanization and cropland expansion were the LCCs with the most significant impacts on LST changes, with urbanization causing a continuous warming effect and cropland expansion consistently leading to cooling, which counteracted each other, resulting in minimal net warming across the region; and (4) The temperature impacts of both urbanization and cropland expansion exhibited a declining trend, primarily driven by non-radiative effects. In summary, this study provides a comprehensive analysis of the spatial distribution, temporal trends, and underlying mechanisms of LCC-driven temperature effects in the NM region, offering valuable insights for future land management policies.</div></div>","PeriodicalId":50839,"journal":{"name":"Agricultural and Forest Meteorology","volume":"372 ","pages":"Article 110667"},"PeriodicalIF":5.7000,"publicationDate":"2025-06-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Temporal trends in biophysical temperature responses to actual land cover changes in northern mid-latitudes from 2006 to 2019\",\"authors\":\"Xuanwei He , Xiangyang Liu , Jing Li , Yitao Li , Wenping Yu , Zhao-Liang Li\",\"doi\":\"10.1016/j.agrformet.2025.110667\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>The biophysical effects of land cover change (LCC) on land surface temperature (LST) have garnered increasing attention. However, previous studies mainly focused on their spatial patterns, leaving temporal trends relatively underexplored. In this study, we selected the densely populated northern mid-latitudes region (NM, 20°N-50°N) as study area, and analyzed the temporal trends in biophysical temperature effects of LCC using long-term satellite observations. The key findings are as follows: (1) from 2006 to 2019, five dominant types of LCC were identified in the NM region, including conversion from barren land to grassland, grassland to barren land, cropland loss, urbanization, and cropland expansion; (2) although the net temperature effect of all LCCs during the study period was relatively small (0.003 K with a declining trend of -0.012 K/decade), this reflected the offsetting impacts of different LCC types, highlighting the importance of analyzing their distinct biophysical effects; (3) urbanization and cropland expansion were the LCCs with the most significant impacts on LST changes, with urbanization causing a continuous warming effect and cropland expansion consistently leading to cooling, which counteracted each other, resulting in minimal net warming across the region; and (4) The temperature impacts of both urbanization and cropland expansion exhibited a declining trend, primarily driven by non-radiative effects. In summary, this study provides a comprehensive analysis of the spatial distribution, temporal trends, and underlying mechanisms of LCC-driven temperature effects in the NM region, offering valuable insights for future land management policies.</div></div>\",\"PeriodicalId\":50839,\"journal\":{\"name\":\"Agricultural and Forest Meteorology\",\"volume\":\"372 \",\"pages\":\"Article 110667\"},\"PeriodicalIF\":5.7000,\"publicationDate\":\"2025-06-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Agricultural and Forest Meteorology\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0168192325002874\",\"RegionNum\":1,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"AGRONOMY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Agricultural and Forest Meteorology","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0168192325002874","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"AGRONOMY","Score":null,"Total":0}
Temporal trends in biophysical temperature responses to actual land cover changes in northern mid-latitudes from 2006 to 2019
The biophysical effects of land cover change (LCC) on land surface temperature (LST) have garnered increasing attention. However, previous studies mainly focused on their spatial patterns, leaving temporal trends relatively underexplored. In this study, we selected the densely populated northern mid-latitudes region (NM, 20°N-50°N) as study area, and analyzed the temporal trends in biophysical temperature effects of LCC using long-term satellite observations. The key findings are as follows: (1) from 2006 to 2019, five dominant types of LCC were identified in the NM region, including conversion from barren land to grassland, grassland to barren land, cropland loss, urbanization, and cropland expansion; (2) although the net temperature effect of all LCCs during the study period was relatively small (0.003 K with a declining trend of -0.012 K/decade), this reflected the offsetting impacts of different LCC types, highlighting the importance of analyzing their distinct biophysical effects; (3) urbanization and cropland expansion were the LCCs with the most significant impacts on LST changes, with urbanization causing a continuous warming effect and cropland expansion consistently leading to cooling, which counteracted each other, resulting in minimal net warming across the region; and (4) The temperature impacts of both urbanization and cropland expansion exhibited a declining trend, primarily driven by non-radiative effects. In summary, this study provides a comprehensive analysis of the spatial distribution, temporal trends, and underlying mechanisms of LCC-driven temperature effects in the NM region, offering valuable insights for future land management policies.
期刊介绍:
Agricultural and Forest Meteorology is an international journal for the publication of original articles and reviews on the inter-relationship between meteorology, agriculture, forestry, and natural ecosystems. Emphasis is on basic and applied scientific research relevant to practical problems in the field of plant and soil sciences, ecology and biogeochemistry as affected by weather as well as climate variability and change. Theoretical models should be tested against experimental data. Articles must appeal to an international audience. Special issues devoted to single topics are also published.
Typical topics include canopy micrometeorology (e.g. canopy radiation transfer, turbulence near the ground, evapotranspiration, energy balance, fluxes of trace gases), micrometeorological instrumentation (e.g., sensors for trace gases, flux measurement instruments, radiation measurement techniques), aerobiology (e.g. the dispersion of pollen, spores, insects and pesticides), biometeorology (e.g. the effect of weather and climate on plant distribution, crop yield, water-use efficiency, and plant phenology), forest-fire/weather interactions, and feedbacks from vegetation to weather and the climate system.