植物生态学报 ›› 2011, Vol. 35 ›› Issue (8): 853-863.DOI: 10.3724/SP.J.1258.2011.00853
所属专题: 青藏高原植物生态学:遥感生态学
宋春桥1,2,4, 游松财3,*(), 柯灵红1,2, 刘高焕1, 钟新科1,2
收稿日期:
2011-03-18
接受日期:
2011-05-17
出版日期:
2011-03-18
发布日期:
2011-07-28
通讯作者:
游松财
作者简介:
*E-mail: yousc@ieda.org.cn
SONG Chun-Qiao1,2,4, YOU Song-Cai3,*(), KE Ling-Hong1,2, LIU Gao-Huan1, ZHONG Xin-Ke1,2
Received:
2011-03-18
Accepted:
2011-05-17
Online:
2011-03-18
Published:
2011-07-28
Contact:
YOU Song-Cai
摘要:
利用遥感数据提取的植被物候格局及时空变化特征能很好地反映区域尺度上植被对全球变化的响应。目前关于青藏高原地区植被物候的少量报道基本上是基于物候站点的观测记录展开分析的。该文基于非对称高斯拟合算法重建了藏北高原2001-2010年的MODIS EVI (增强型植被指数)时间序列影像, 然后利用动态阈值法提取整个藏北高原2001-2010年植被覆盖的重要物候信息, 包括植被返青期、枯黄期与生长季长度, 分析了植被物候10年间平均状况的空间分异特征以及年际变化情况, 并结合站点观测记录分析了气温和降水对植被物候变化的影响, 结果表明: (1)藏北高原植被返青期在空间上表现出从东南到西北逐渐推迟的水平地带性与东南高山峡谷区的垂直地带性相结合的特征, 近60%区域的植被返青期提前, 特别是高山地区; (2)植被枯黄期的年际变化不太明显, 大部分地区都表现为自然的年际波动; (3)生长季长度的时空变化特征由植被返青期和枯黄期二者决定, 但主要受返青期提前影响, 大部分地区生长季长度延长; (4)研究区内不同气候区划植被物候的年际变化以那曲高山谷地亚寒带半湿润区和青南高原亚寒带半干旱区的植被返青期提前和生长季延长程度最为明显; (5)基于气象台站数据分析气候变化对物候的影响发现, 返青期提前及生长季延长主要受气温升高的影响, 与降水的关系尚不明确。
宋春桥, 游松财, 柯灵红, 刘高焕, 钟新科. 藏北高原植被物候时空动态变化的遥感监测研究. 植物生态学报, 2011, 35(8): 853-863. DOI: 10.3724/SP.J.1258.2011.00853
SONG Chun-Qiao, YOU Song-Cai, KE Ling-Hong, LIU Gao-Huan, ZHONG Xin-Ke. Spatio-temporal variation of vegetation phenology in the Northern Tibetan Plateau as detected by MODIS remote sensing. Chinese Journal of Plant Ecology, 2011, 35(8): 853-863. DOI: 10.3724/SP.J.1258.2011.00853
图2 基于像元时间序列曲线的物候指标提取原理。NDVI, 归一化植被指数。
Fig. 2 Principle of extracting phenological metrics based on time-series curve of pixels. NDVI, normalized difference vegetation index.
图3 2001-2010年藏北高原植被的平均返青期(A)及其年际变化(B)。
Fig. 3 Average greenup date of growing season (A) and inter-annual variation (B) of vegetation in Northern Tibetan Plateau between 2001-2010.
图5 2001-2010年藏北高原植被平均生长季长度(A)及其年际变化(B)。
Fig. 5 Average length of growing season (A) and its inter-annual variation (B) of vegetation in Northern Tibetan Plateau between 2001-2010.
图4 2001-2010年藏北高原植被平均枯黄期期(A)及其年际变化(B)。
Fig. 4 Average senescence date of growing season (A) and its inter-annual variation (B) of vegetation in Northern Tibetan Plateau between 2001-2010.
图6 藏北高原不同气候区植被物候的年际变化。DOY, 年序日。A、B、C、D分别为气候区划昆仑高山亚寒带干旱区、羌塘高原湖盆亚寒带半干旱区、那曲高山谷地亚寒带半湿润区和青南高原亚寒带半干旱区的植被物候。
Fig. 6 Inter-annual changes of vegetation phenology in four different climate zones over Northern Tibetan Plateau. DOY, day of year. A, B, C and D show vegetation phenology in four climate zones which respectively refer to Kunlun mountain subfrigid and arid zone, Qiangtang plateau and lake-basin subfrigid and semi-arid zone, Nagqu mountain and valley subfrigid and semi-humid zone, and south Qinghai plateau subfrigid and semi-arid zone, respectively.
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