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秦岭太白红杉林遥感物候提取及对气候变化的响应

郭少壮1,2,白红英1,2*,黄晓月1,2,孟清1,2,赵婷1,2   

  1. 1西北大学城市与环境学院, 西安 710127; 2陕西省地表系统与环境承载力重点研究室, 西安 710127)
  • 出版日期:2019-04-10 发布日期:2019-04-10

Remote sensing phenology of Larix chinensis forest in response to climate change in Qinling Mountains.

GUO Shao-zhuang1,2, BAI Hong-ying1,2*, Huang Xiao-yue1,2, Meng Qing1,2, Zhao Ting1,2   

  1. (1College of Urban and Environmental Science, Northwest University, Xi’an, 710127, China; 2Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, Northwest University, Xi’an, 710127, China).
  • Online:2019-04-10 Published:2019-04-10

摘要: 高山林线树种对气候变化响应敏感,是研究气候变化和物候变化的理想树种。本文基于双Logistic曲线拟合法重建了2000—2015年MODIS EVI2时间序列影像并提取太白红杉林关键物候参数,结合太白山地区气象站的气候资料,研究太白红杉林遥感物候及其对气候因子的响应。结果表明:2000—2015年太白红杉林生长期开始时间在第120天左右,生长期结束时间在第288天左右,平均生长期长度为168 d;16 a来太白红杉林生长期始期整体呈提前趋势,变化率为-0.65 d·10 a-1;生长期末期整体呈推迟趋势,变化率为0.35 d·10 a-1;整个生长期呈延长趋势,平均延长幅度为0.99 d·10 a-1;太白红杉林物候始期与同期气温、降水呈负相关的区域分别占研究区的73.11%和61.25%,而与潜在蒸散呈正相关的区域占65.17%;物候末期与同期气温、降水、潜在蒸散、日照和风速均呈正相关,面积比分别为74.91%、72.87%、78.14%、68.60%和64.74%,其中气温是太白红杉林物候始期提前的主要影响因素,气温、降水、潜在蒸散是物候末期推迟的主要影响因素。

关键词: 高山森林, 凋落物分解, 释放动态, 雪被斑块

Abstract: Tree species at alpine timberline are sensitive to climate change, which are ideal species for studying climate change and phenological change. Based on the double Logistic curve fitting method, we reconstructed the MODIS EVI2 time series images from 2000 to 2015 and extracted key phenological parameters of Larix chinensis forest, combined with climatic data of the Taibai Mountain meteorological station, and analyzed the phenology of the L. chinensis forest and its responses to climate factors. From 2000 to 2015, the beginning time of growing period of L. chinensis forest was on about 120th day, and the ending time of growth period was on about 288th day, with an average growing period of 168 days. The rate of change was -0.65 d·10 a-1 at the beginning of the growing season with an advanced trend, and it was 0.35 d·10 a-1 at the end of the growing season with a delayed trend, with a delayed trend of 0.99 d·10 a-1 for the whole growing season. The areas with negative correlation between the start phenophase of L. chinensis forest and the temperature and precipitation in the same period accounted for 73.11% and 61.25% of the study area, respectively, while the areas with positive correlation between the start phenophase and the potential evapotranspiration accounted for 65.17% of the study area. The end of phenophase was positively correlated with temperature, precipitation, potential evapotranspiration, sunshine and wind speed in the same period, with area rates of 74.91%, 72.87%, 78.14%, 68.60% and 64.74%, respectively. Temperature was the major factor affecting the advance of the phenological stage of L. chinensis forest, while temperature, precipitation and potential evapotranspiration were the major factors affecting the late phenology.

Key words: alpine forest, litter decomposition, dynamic of release, snow patch.