生态与农村环境学报 ›› 2014, Vol. 30 ›› Issue (4): 423-429.doi:

• 区域环境与发展 • 上一篇    下一篇

近12年陕甘宁黄土高原区植被物候时空变化特征

韦振锋,王德光,张翀,刘炎序   

  1. 陕西师范大学旅游与环境学院
  • 收稿日期:2013-11-26 修回日期:2014-06-09 出版日期:2014-07-25 发布日期:2014-10-11
  • 通讯作者: 王德光 陕西师范大学旅游与环境学院 E-mail:116690728@qq.com
  • 作者简介:韦振锋(1983—),男,广西东兰人,讲师,博士生,主要研究方向为GIS 与国土资源评价。E-mail:weizhenfeng112@163.com
  • 基金资助:

    国家自然科学基金(71361001)

Spatio-Temporal Variation of Vegetation Phenology on Loess Plateau in Shaanxi-Gansu- Ningxia Region in Recent 12 Years

WEI  Zhen-Feng, WANG  De-Guang, ZHANG  Chong, LIU  Yan-Xu   

  1. College of Tourism and Environment,Shaanxi Normal University
  • Received:2013-11-26 Revised:2014-06-09 Online:2014-07-25 Published:2014-10-11
  • Contact: WANG De-Guang College of Tourism and Environment,Shaanxi Normal University E-mail:116690728@qq.com

摘要: 以SPOT VEGETATION旬数据集为数据源,研究1999-2010年陕甘宁黄土高原区植被物候时空特征。采用时间序列谐波分析法对原数据进行预处理,通过傅里叶插值法将NDVI旬数据插值成日数据,再通过阈值法和最大比率法确定植被物候期。结果表明,陕甘宁黄土高原地区植被物候多年平均值呈纬度变化规律,纬度低的地区生长季始期(SOG)和生长季末期(EOG)提前,生长季长度(LOG)缩短。海拔高度每上升100m,SOG提前约3d(P<0.01),EOG提前约2d(P<0.01), LOG延长约1d(P>0.05)。1999-2010年植被SOG、EOG和LOG的物候年际变化率分别为-0.02、0.003和0.002 d·a-1。陕甘宁大部分地区SOG呈提前趋势,EOG呈推迟趋势,LOG呈延长趋势。植物物候与降水和河流网相关,干旱低温高纬度地区植被生长停滞提前,生长周期缩短。

关键词: 黄土高原区, 植被物候, 生长季始期, 生长季末期, 生长季长度

Abstract: Based on a ten-year (1999-2010) SPOT VEGETATION dataset, spatio-temporal vegetation phonological phenological features on the Shaan-Gan-Ning Loess Plateau were studied. The method of harmonic analysis of time series (HANTS) was adopted to pre-process the raw data, the fourier interpolation method to turn NDVI ten-day data into daily data, and the threshold value method and the maximum ratio method to specify vegetation phonological phenological phases. Results show that the multi-year average of vegetation phenology space distribution in the Shanxi-Gansu-Ningxia Region varied with the latitude, that is to say, the lower the latitude, the relatively earlier the growth season started (SOG) and ended (EOG)and the shorter the growth season (LOG). Moreover, it started 3 days earlier (P<0.01), ended two days earlier (P<0.01), and lasted one day longer (P>0.05) with the attitude rising every 100 m. During the ten ten-year period (1999 – 2010), the annual rate of change in vegetation phenology, SOG, EOGand LOG in that region, was -0.02, 0.003 and 0.02 d?a-1, respectively. The vegetation phenology in most part of the Loess Plateau tended to have SOG advanced, EOG postponed and LOG extended, which were supposed to be related to variation of precipitation and the river net system. In high latitude regions, arid and low in temperature, vegetation growth started stagnation earlier and shortened in life cycle.

Key words: Loess Plateau region, vegetation phenology, SOG, EOG, LOG

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