Phenological changes of desert steppe vegetation and its effect on net primary productivity in Inner Mongolia from 2000 to 2017

Xiaoyu DONG; Huarong YAO; Junhu DAI; Mengyao ZHU

doi:10.18306/dlkxjz.2020.01.003

[1] [M]. Summary for policymakers. Climate change 2013: The physical science basis, contribution of working group i to the fifth assessment report of the intergovernmental panel on climate change(2013).

[3] Sparks T H, Menzel A. Observed changes in seasons: An overview[J]. International Journal of Climatology, 22, 1715-1725(2002).

[5] Ge Q S, Wang H J, Rutishauser T et al. Phenological response to climate change in China: A meta-analysis[J]. Global Change Biology, 21, 265-274(2015).

[7] Piao S L, Fang J Y, Zhou L M et al. Variations in satellite-derived phenology in China's temperate vegetation[J]. Global Change Biology, 12, 672-685(2006).

[11] Sha Z Y, Zhong J L, Bai Y F et al. Spatio-temporal patterns of satellite-derived grassland vegetation phenology from 1998 to 2012 in Inner Mongolia, China[J]. Journal of Arid Land, 8, 462-477(2016).

[12] Gong Z, Kawamura K, Ishikawa N et al. MODIS normalized difference vegetation index (NDVI) and vegetation phenology dynamics in the Inner Mongolia grassland[J]. Solid Earth, 6, 1185-1194(2015).

[13] Myneni R B, Keeling C D, Tucker C J et al. Increased plant growth in the northern high latitudes from 1981 to 1991[J]. Nature, 386, 698-702(1997).

[14] Field C B, Behrenfeld M J, Randerson J T et al. Primary production of the biosphere: Integrating terrestrial and oceanic components[J]. Science, 281, 237-240(1998).

[19] Piao S L, Friedlingstein P, Ciais P et al. Growing season extension and its impact on terrestrial carbon cycle in the Northern Hemisphere over the past 2 decades[J]. Global Biogeochemical Cycles, 21, 1-11(2007).

[20] Richardson A D, Black T A, Ciais P et al. Influence of spring and autumn phenological transitions on forest ecosystem productivity[J]. Philosophical Transactions of the Royal Society of London, 365, 3227-3246(2010).

[21] Piao S L, Ciais P, Friedlingstein P et al. Net carbon dioxide losses of northern ecosystems in response to autumn warming[J]. Nature, 451, 49-52(2008).

[28] Liu R G, Liu Y. Generation of new cloud masks from MODIS land surface reflectance products[J]. Remote Sensing of Environment, 133, 21-37(2013).

[29] Yang K. China meteorological forcing data (1979-2018)[EB/OL]. Big Data System for Pan-Third Pole(2018).

[31] Jonsson P, Eklundh L. Seasonality extraction by function fitting to time-series of satellite sensor data[J]. IEEE Transactions on Geoscience & Remote Sensing, 40, 1824-1832(2002).

[32] Wang S Y, Zhang B, Yang Q C et al. Responses of net primary productivity to phenological dynamics in the Tibetan Plateau, China[J]. Agricultural & Forest Meteorology, 232, 235-246(2017).

[34] Potter C S, Randerson J T, Field C B et al. Terrestrial ecosystem production: A process model based on global satellite and surface data[J]. Global Biogeochemical Cycles, 7, 811-841(1993).

[38] Tao Z X, Wang H J, Liu Y C et al. Phenological response of different vegetation types to temperature and precipitation variations in northern China during 1982-2012[J]. International Journal of Remote Sensing, 38, 3236-3252(2017).

[45] Richardson A D, Anderson R S, Arain M A et al. Terrestrial biosphere models need better representation of vegetation phenology: Results from the North American carbon program site synjournal[J]. Global Change Biology, 18, 566-584(2012).

[46] Wu C Y, Chen J M, Gonsamo A et al. Interannual variability of net carbon exchange is related to the lag between the end-dates of net carbon uptake and photosynjournal: Evidence from long records at two contrasting forest stands[J]. Agricultural and Forest Meteorology, 164, 29-38(2012).