地球信息科学学报 ›› 2019, Vol. 21 ›› Issue (5): 767-780.doi: 10.12082/dqxxkx.2019.180578
出版日期:
2019-05-25
发布日期:
2019-05-25
通讯作者:
阎世杰
E-mail:yansj@radi.ac.cn
作者简介:
作者简介:阎世杰(1994-),男,湖北宜昌人,硕士,研究方向为遥感图像处理,深度学习等。E-mail:
基金资助:
Shijie YAN1,2,*(), Huan WANG2,3, Kewei JIAO4
Online:
2019-05-25
Published:
2019-05-25
Contact:
Shijie YAN
E-mail:yansj@radi.ac.cn
Supported by:
摘要:
作为气候变化的敏感指示器,植被的物候、生长、空间分布格局等特征及其动态变化主要取决于气候环境中的水热条件,因此在气候变化背景下,气候-植被关系成为了全球变化研究的前沿和热点问题。本文综合平均温度、降水、水汽压、湿度、日照时数、SPEI等气候因子,坡度、坡向海拔等地形因子及人为活动因子,应用地理探测器方法针对2006-2015年京津冀地区不同季节NDVI、不同地貌类型区、不同植被类型区生长季NDVI的定量归因研究,揭示了过去10年间植被时空分布格局,及植被对气候、非气候因素响应的季节差异与区域差异,以期为生态工程的建设与修复提供参考意义。趋势分析表明:①2006-2015年京津冀地区NDVI呈现增加趋势,但存在显著的空间差异,如山地生长季NDVI的增长速率大于平原、台地、丘陵等地;②基于地理探测器的定量归因结果表明,降水是年尺度上NDVI空间分布的主导因子(解释力39.4%),土地利用与降水的交互作用对NDVI的影响最为明显(q=58.2%);③NDVI对气候因子的响应存在季节性及区域性差异,水汽压是春季NDVI空间分布的主导因子,湿度是夏、秋两季的主导因子,土地利用是冬季的主导因子;④影响因子对生长季NDVI的解释力因不同地貌类型区、不同植被类型区而差异显著。
阎世杰, 王欢, 焦珂伟. 京津冀地区植被时空动态及定量归因[J]. 地球信息科学学报, 2019, 21(5): 767-780.DOI:10.12082/dqxxkx.2019.180578
Shijie YAN, Huan WANG, Kewei JIAO. Spatiotemporal Dynamics of NDVI in the Beijing-Tianjin-Hebei Region based on MODIS Data and Quantitative Attribution[J]. Journal of Geo-information Science, 2019, 21(5): 767-780.DOI:10.12082/dqxxkx.2019.180578
表1
研究数据、数据来源及计算方法"
需要的数据 | 数据来源 | 计算方法 |
---|---|---|
MODIS中国NDVI月合成数据(2006.01-2015.12) | 中国科学院计算机网络信息中心国际科学数据镜像网站(http://www.gscloud.cn) | |
气象数据(降水、平均温度、最高温度、最低温度、风速、日照时数、湿度和水汽压) | 国家气象信息中心(http://data.cma.cn) | 其中水汽压数据由湿度数据计算得到 |
标准化降水蒸散指数(SPEI) | 由常规气象数据计算得到 | SPEI采用Beguería 等[ |
30m、1000mDEM数据 | 中国科学院资源环境科学数据中心(http://www.resdc.cn) | |
植被类型数据(1:100万)[ | 中国科学院资源环境科学数据中心(http://www.resdc.cn) | |
地貌类型数据(1:100万) | 中国科学院资源环境科学数据中心(http://www.resdc.cn) | |
土地利用数据(2005, 2010, 2015) | 中国科学院资源环境科学数据中心(http://www.resdc.cn) |
表5
2006-2015年京津冀地区不同地貌形态类型区生长季NDVI影响因子交互作用q值"
平原 | 台地 | 丘陵 | 小起伏山地 | 中起伏山地 | 大起伏山地 | |
---|---|---|---|---|---|---|
主导交互作用1 | 日照时数∩水汽压 | 湿度∩日照时数 | 平均温度∩湿度 | 降水∩土地利用 | 湿度∩土地利用 | 土地利用∩降水 |
q值 | 0.586 | 0.755 | 0.760 | 0.634 | 0.587 | 0.570 |
主导交互作用2 | 日照时数∩湿度 | 湿度∩干旱指数 | 降水∩土地利用 | 湿度∩土地利用 | 降水∩土地利用 | 土地利用∩湿度 |
q值 | 0.575 | 0.744 | 0.758 | 0.606 | 0.579 | 0.513 |
主导交互作用3 | 降水∩湿度 | 湿度∩土地利用 | 日照时数∩湿度 | 湿度∩平均温度 | 湿度∩日照时数 | 降水∩海拔 |
q值 | 0.539 | 0.743 | 0.750 | 0.596 | 0.502 | 0.485 |
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