Intercomparison, interpretation, and assessment of spring phenology in North America estimated from remote sensing for 1982-2006

被引:882
作者
White, Michael A. [1 ]
de Beurs, Kirsten M. [2 ]
Didan, Kamel [3 ]
Inouye, David W. [4 ]
Richardson, Andrew D. [5 ]
Jensen, Olaf P. [6 ]
O'Keefe, John [7 ]
Zhang, Gong [1 ]
Nemani, Ramakrishna R. [8 ]
van Leeuwen, Willem J. D. [9 ,10 ]
Brown, Jesslyn F. [11 ]
de Wit, Allard [12 ]
Schaepman, Michael [12 ]
Lin, Xioamao [13 ]
Dettinger, Michael [14 ]
Bailey, Amey S. [15 ]
Kimball, John [16 ]
Schwartz, Mark D. [17 ]
Baldocchi, Dennis D. [18 ]
Lee, John T. [19 ]
Lauenroth, William K. [20 ,21 ]
机构
[1] Utah State Univ, Dept Watershed Sci, Logan, UT 84322 USA
[2] Virginia Polytech Inst & State Univ, Dept Geog, Blacksburg, VA 24061 USA
[3] Univ Arizona, Inst Study Planet Earth, Tucson, AZ USA
[4] Univ Maryland, Dept Biol, College Pk, MD 20742 USA
[5] Univ New Hampshire, Complex Syst Res Ctr, Durham, NH 03824 USA
[6] Univ Wisconsin, Ctr Limnol, Madison, WI 53706 USA
[7] Harvard Forest, Petersham, MA USA
[8] NASA, Ames Res Ctr, Moffett Field, CA 94035 USA
[9] Univ Arizona, Off Arid Lands Studies, Tucson, AZ USA
[10] Univ Arizona, Dept Geog & Reg Dev, Tucson, AZ USA
[11] Earth Resources Observat & Sci EROS Ctr, US Geol Survey, Land Sci Div, Sioux Falls, SD USA
[12] Wageningen UR, Ctr Geoinformat, Wageningen, Netherlands
[13] Campbell Sci Inc, Logan, UT USA
[14] Univ Calif San Diego, Scripps Inst Oceanog, US Geol Survey, La Jolla, CA 92093 USA
[15] Hubbard Brook Expt Forest, Campton, NH USA
[16] Univ Montana, Flathead Lake Biol Stn, Div Biol Sci, Polson, MT 59860 USA
[17] Univ Wisconsin, Dept Geog, Milwaukee, WI 53201 USA
[18] Univ Calif Berkeley, Dept Environm Sci Policy & Management, Berkeley, CA 94720 USA
[19] Univ Maine, Dept PSE, Environm Phys Grp, Orono, ME USA
[20] Colorado State Univ, Grad Degree Program Ecol, Ft Collins, CO 80523 USA
[21] Colorado State Univ, Warner Coll Nat Resources, Ft Collins, CO 80523 USA
基金
美国国家科学基金会;
关键词
bloom; budburst; climate change; flower; growing season; land surface phenology; seasonality; NDVI TIME-SERIES; PLANT PHENOLOGY; CLIMATE-CHANGE; FOURIER-ANALYSIS; TRENDS; VARIABILITY; RESPONSES; EARLIER; COVER; ONSET;
D O I
10.1111/j.1365-2486.2009.01910.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Shifts in the timing of spring phenology are a central feature of global change research. Long-term observations of plant phenology have been used to track vegetation responses to climate variability but are often limited to particular species and locations and may not represent synoptic patterns. Satellite remote sensing is instead used for continental to global monitoring. Although numerous methods exist to extract phenological timing, in particular start-of-spring (SOS), from time series of reflectance data, a comprehensive intercomparison and interpretation of SOS methods has not been conducted. Here, we assess 10 SOS methods for North America between 1982 and 2006. The techniques include consistent inputs from the 8 km Global Inventory Modeling and Mapping Studies Advanced Very High Resolution Radiometer NDVIg dataset, independent data for snow cover, soil thaw, lake ice dynamics, spring streamflow timing, over 16 000 individual measurements of ground-based phenology, and two temperature-driven models of spring phenology. Compared with an ensemble of the 10 SOS methods, we found that individual methods differed in average day-of-year estimates by +/- 60 days and in standard deviation by +/- 20 days. The ability of the satellite methods to retrieve SOS estimates was highest in northern latitudes and lowest in arid, tropical, and Mediterranean ecoregions. The ordinal rank of SOS methods varied geographically, as did the relationships between SOS estimates and the cryospheric/hydrologic metrics. Compared with ground observations, SOS estimates were more related to the first leaf and first flowers expanding phenological stages. We found no evidence for time trends in spring arrival from ground- or model-based data; using an ensemble estimate from two methods that were more closely related to ground observations than other methods, SOS trends could be detected for only 12% of North America and were divided between trends towards both earlier and later spring.
引用
收藏
页码:2335 / 2359
页数:25
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