Growing season extension and its impact on terrestrial carbon cycle in the Northern Hemisphere over the past 2 decades

By Shilong Piao, Pierre Friedlingstein, Philippe Ciais, N. Viovy, J. Demarty. 2007

763 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/b6d549e9dfcf1cf4239fb9e2938f0032ea7030d4

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In Global and Planetary Change

Citations in the corpus

Phenology shifts at start vs. end of growing season in temperate vegetation over the Northern Hemisphere for the period 1982–2008 (2011, background): “Because the changes in GPP and NPP are a main factor in modulating terrestrial carbon uptake, changes in the growing season can have a critical influence on the variations in atmospheric carbon magnitude or content (Nemani et al., 2002; Piao et al., 2007).”
Sand and Dust Storms: Impact Mitigation (2017, background): “The GGW program has greatly improved vegetation cover and effectively reduced dust storm intensity in parts of northern China [8], but other researchers point to warmer temperatures and greater rainfall as being more important drivers of greening trends in the area [146], and the value of large-scal”
Factors Affecting Long-Term Trends in Global NDVI (2019, background): “The negative correlation m y be caused by an increa e in the evaporation of soil moisture resulting from the rise in temperature, which then leads to the decline of soil moisture; in this case, the ‘physiological drought’ of plants occurs and limits the photosynthesis and growth rate of plants [40].”
Solar park microclimate and vegetation management effects on grassland carbon cycling (2016, background): “…processes, different microclimate metrics should be analysed, including averages, minimum and maximum temperatures (Jolly et al 2005, Craine et al 2012), along with seasonal variation, encapsulated by measures of growing season length, and diurnal variation (Piao et al 2007,Wan et al 2009).”
Detection and attribution of vegetation greening trend in China over the last 30 years (2015, background): “It has been suggested that this warming has stimulated vegetation growth both through extending the growing season and through promoting summer photosynthesis, particularly in regions where water is nonlimiting (Niemand et al., 2005; Piao et al., 2007, 2008).”
Evaluation of terrestrial carbon cycle models for their response to climate variability and to CO2 trends (2013, neutral): “This implies that rising MAT causes an extension of the growing season, and induces an increase in GPP (Piao et al., 2007; Richardson et al., 2010) during warm years.”
Green-up dates in the Tibetan Plateau have continuously advanced from 1982 to 2011 (2013, background): “A prolonged growing season (due to earlier SOS) can potentially enhance the carbon sink capacity of terrestrial ecosystems, which has been shown in terrestrial ecosystems in the northern mid and higher latitudes during 1980–2002 (26).”
Plant phenology and global climate change: Current progresses and challenges (2019, background): “Modeling studies have shown that an exten‐ sion of 1‐day in growing season length can increase annual GPP of northern ecosystems by 0.5%–0.6% (Piao et al., 2007; White et al., 2009).”
Recent changes in phenology over the northern high latitudes detected from multi-satellite data (2011, background): “Moreover, gross primary production (GPP) and net ecosystem production (NEP) are closely related to growing season dynamics and are key factors in the terrestrial carbon budget (Piao et al 2007).”