Chen Huailiang, Liu Yujie, Du Zixuan, et al. The change of growing season of the vegetation in Huanghe-Huaihe-Haihe Region and its responses to climate changes. J Appl Meteor Sci, 2011, 22(4): 437-444.
Citation: Chen Huailiang, Liu Yujie, Du Zixuan, et al. The change of growing season of the vegetation in Huanghe-Huaihe-Haihe Region and its responses to climate changes. J Appl Meteor Sci, 2011, 22(4): 437-444.

The Change of Growing Season of the Vegetation in Huanghe-Huaihe-Haihe Region and Its Responses to Climate Changes

  • Received Date: 2010-12-16
  • Rev Recd Date: 2011-05-19
  • Publish Date: 2011-08-31
  • Using the each ten-day data of NOAA/AVHRR from 1981 to 2000 and adopting the Maximum-Slope method, Curve-Fitting method and stepwise regression, the beginning and ending of the growth season of the vegetations in the Huanghe-Huaihe-Haihe (HHH) region are analyzed. Meanwhile, the pixel by pixel INDV map is worked out with typical bands as the sample. Through analyzing the change of green wave and brown wave, the changing rules of vegetation activities and its responses to climate changes in the past 20 years are revealed. The growth season in HHH region starts at the last 10 days of March with INDV 0.19604 and ends at the first 10 days of November with INDV 0.22899 on average. The tendency is that the growing season has prolonged obviously by starting earlier and earlier, while ending later and later from 1982 to 2000. The average INDV for the vegetation in the researched area in the past 20 years is generally increasing, especially in spring. According to the INDV map of typical bands as the sample worked out with the pixel by pixel, the green wave changes from south to north during January—July on the band of 116°E, the maximum of INDV occurs in August and decreases gradually after September. On the band of 36°N, to the east and nearby 116°E, the INDV has two peaks because of two crops a year, which is obviously different from other regions. The two peaks occur in April and August and they become clearer and clearer from 1982 to 2000, especially in agriculture area. However, the two peaks are not obvious to the north of 38.5°N, in the area of Beijing, Tianjin and the mountain areas, and the peak value of early summer is lower than that of autumn. In agriculture area, the peak interval of green wave is broadening with the time passing by, and it's more obviously from south to north. With the time passing by, the green wave of the critical value of the growth season in the area changes from south to north, while the emergence of brown wave prolongs from north to south. According to the stepwise regression result of the every ten-day meteorological data and the INDV of the typical sampling areas in the HHH region, the INDV of vegetation is closely related to the temperature and precipitation, especially it's more sensitive to the temperature, and the significance of the correlation is 0.01. The prolonging of vegetation growth season is a main response to climate changes of vegetation activities in target areas.
  • Fig. 1  Multi-year average NDVI ten-day changing curve (a) and changing slope curve (b)

    Fig. 2  Multi fitting of multi-year average NDVI ten-day changing curve

    Fig. 3  Changing curve on the beginning time (a) and ending time (b) of growth season from 1982 to 2000

    Fig. 4  Cross section of vegetation index changing in 116°E meridional band (a) and 36°N zonal band (b) during 1982—2000

    Fig. 5  Cross section of vegetation index changing in 116°E meridional band (a) and 36°N zonal band (b) during 1982—2000

    Fig. 6  Average INDV changes of vegetations in different seasons from 1982 to 2000

    Fig. 7  Annual INDV changing curve of vegetations (a) and vegetations in the last 10 days of March (b) in target areas

    Table  1  Relativity index of each ten-day average INDV of vegetations in target areas and the ten-day climate factors

    植被类型 温度 降水
    农田 0.538* 0.304*
    落叶阔叶林 0.894* 0.435*
     注:*表示通过α=0.01的显著性检验。
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  • [1]
    王长耀, 牛铮, 张庆员, 等.利用NOAA NDVI数据集分析中国植被绿波推移规律.中国图象图形学报, 1999, 4(11):976-979. doi:  10.3969/j.issn.1006-8961.1999.11.014
    [2]
    方修琦, 余卫红.物候对全球变暖响应的研究综述.地球科学进展, 2002, 17(5):714-719. http://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ200205014.htm
    [3]
    崔读昌.气候变暖对水稻生育期影响的情景分析.应用气象学报, 1995, 6(3):361-365. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19950356&flag=1
    [4]
    裘国旺, 王馥棠.气候变化对我国江南双季稻生产可能影响的数值模拟研究.应用气象学报, 1998, 9(2):151-159. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19980222&flag=1
    [5]
    Myneni R B, Tucker C J, Asar G, et al. Interannual variations in satellite-sensed vegetation index data from 1981 to 1991. J Geophys Res, 1998, 103(D6): 6145-6160. doi:  10.1029/97JD03603
    [6]
    Zhou L M, Tucker C J, Kaufmann R K, et al. Variations in northern vegetation activity inferred from satellite data of vegetation index during 1981 to 1999. J Geophys Res, 2001, 106(D17): 20069-20083. doi:  10.1029/2000JD000115
    [7]
    Keeling C D, Chin J F S, Whorf T P. Increased activity of northern vegetation in inferred from atmospheric CO2 measurements. Nature, 1996, 382:146-149. doi:  10.1038/382146a0
    [8]
    李红梅, 马玉寿, 王彦龙.气候变暖对青海高原地区植物物候期的影响.应用气象学报, 2010, 21(4):500-505. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20100414&flag=1
    [9]
    朴世龙, 方精云.1982—1999年我国陆地植被活动对气候变化响应的季节差异.地理学报, 2003, 58(1):119-125. doi:  10.11821/xb200301014
    [10]
    杜子璇, 陈怀亮, 刘忠阳.黄淮海地区植被覆盖变化驱动力与驱动机制研究.气象与环境科学, 2007, 30(3):3-7. http://www.cnki.com.cn/Article/CJFDTOTAL-HNQX200703000.htm
    [11]
    《中国自然地理》编辑委员会.中国自然地理 (气候).北京:科学出版社, 1984.
    [12]
    中国科学院植物研究所. 1:400万中国植被图.北京:中国地图出版社, 1979.
    [13]
    除多, 德吉央宗, 普布次仁, 等.西藏藏北高原典型植被生长对气候要素变化的响应.应用气象学报, 2007, 18(6):832-839. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=200706125&flag=1
    [14]
    Eleonora Runtunuwu, Akihiko Kondoh, Ketut Wikantika, et al. NDVI-derived length of the growth period estimations for different vegetation types in Monsoon Asia. IECI Chapter Japan Series, 2001, 3(1):106-109.
    [15]
    Eleonora Runtunuwu, Akihiko Kondoh. Length of the growth period derived from remote sensed and climate data for different vegetation types in Monsoon Asia. Indonesian Journal of Agricultural Sciences, 2001, 1: 1-4. https://indonesianagricsci.files.wordpress.com/2007/11/ijas0101.pdf
    [16]
    陈怀亮, 刘玉洁, 杜子璇, 等.基于卫星遥感数据的黄淮海地区植被覆盖时空变化特征.生态学杂志, 2010, 29(5):991-999. http://www.cnki.com.cn/Article/CJFDTOTAL-STXZ201005027.htm
    [17]
    郑有飞, 牛鲁燕, 吴荣军, 等.1982—2003年贵州省植被覆盖变化及其对气候变化的响应.生态学杂志, 2009, 28(9):1773-1778. http://www.cnki.com.cn/Article/CJFDTOTAL-STXZ200909018.htm
    [18]
    陈燕丽, 龙步菊, 潘学标, 等.基于MODIS NDVI和气候信息的草原植被变化监测.应用气象学报, 2010, 21(2):229-236. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20100213&flag=1
    [19]
    史培军, 宫鹏, 李晓兵.土地利用/覆盖变化研究的方法与实践.北京:科学出版社, 2000.
    [20]
    James M E, Kalluri S N V. The pathfinder AVHRR land area data set: An improved coarse resolution data set for terrestrial monitoring. Int J Remote Sens, 1994, 15: 3347-3363. doi:  10.1080/01431169408954335
    [21]
    李本纲, 陶澍. AVHRR NDVI与气候因子的相关分析.生态学报, 2000, 20(5): 898-902. http://www.cnki.com.cn/Article/CJFDTOTAL-STXB200005028.htm
    [22]
    Defries R S, Townshend J R G. NDVI-derived land cover classification at a global scale. Int J Remote Sens, 1994, 15: 3567-3586. doi:  10.1080/01431169408954345
    [23]
    陈怀亮, 徐祥德, 杜子璇, 等.黄淮海地区植被活动对气候变化的响应特征.应用气象学报, 2009, 20(5):513-520. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20090501&flag=1
    [24]
    Groten S M E, Ocatre R. Monitoring the length of the growing season with NOAA. Int J Remote Sens, 2002, 23(14): 2797-2815. doi:  10.1080/01431160110070843
    [25]
    Schwartz M D, Reed B C, White M A. Assessing satellite-derived start-of-season (SOS) measures in the Conterminous USA. International Journal of Climatology, 2002, 22(14): 1793-1805. doi:  10.1002/(ISSN)1097-0088
    [26]
    Hogda K A, Karlsen S R, Solheim I. Climatic Change Impact on Growing Season in Fennoscandia Studied by a Time Series of NOAA AVHRR NDVI Data. Proceedings of IGARSS, 2001:9-13. http://ieeexplore.ieee.org/document/976837/
    [27]
    Yu F, Price K P, Lee R Y, et al. Analysis of the Relationships Between Climatic Variation and Seasonal Vegetation Development in Eastern Central Asia. ASPRS 2000 Annual Conference. Washington D C, 2000.
    [28]
    温刚, 符淙斌.中国东部季风区植被物候季节变化对气候响应的大尺度特征:多年平均结果.大气科学, 2000, 24(5):667-682. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK200005013.htm
    [29]
    王宏, 李晓兵, 莺歌, 等.基于NOAA NDVI的植被生长季模拟方法研究.地理科学进展, 2006, 25(6): 21-32. doi:  10.11820/dlkxjz.2006.06.003
    [30]
    柳晶, 郑有飞, 赵国强, 等.郑州植物物候对气候变化的响应.生态学报, 2007, 27(4): 1471-1479. http://www.cnki.com.cn/Article/CJFDTOTAL-STXB200704025.htm
    [31]
    陈彬彬, 郑有飞, 赵国强, 等.河南林州植物物候变化特征及其原因分析.植物资源与环境学报, 2007, 16(1): 12-17. http://www.cnki.com.cn/Article/CJFDTOTAL-ZWZY200701003.htm
    [32]
    韩秀珍, 李三妹, 罗敬宁, 等.近20年中国植被时空变化研究.干旱区研究, 2008, 25(6): 753-759. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGQX200610012026.htm
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    • Received : 2010-12-16
    • Accepted : 2011-05-19
    • Published : 2011-08-31

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