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Open AccessJournal ArticleDOI

Earlier springs decrease peak summer productivity in North American boreal forests

TLDR
In this paper, the authors analyzed nearly three decades (1982?2008) of observational records and derived products, including satellite microwave and optical imagery as well as upscaled ecosystem flux observations, to better understand how shifts in seasonality impact hydrology and productivity in the North American boreal forests.
Abstract
In the northern high latitudes, alternative hypotheses with regards to how warming-related shifts in seasonality influence ecosystem productivity exist. Increased plant growth associated with a longer growing season may enhance ecosystem productivity, but shifts to earlier springs may also negatively influence soil moisture status and productivity during the peak of the growing season. Here, we analyzed nearly three decades (1982?2008) of observational records and derived products, including satellite microwave and optical imagery as well as upscaled ecosystem flux observations, to better understand how shifts in seasonality impact hydrology and productivity in the North American boreal forests. We identified a dominant adverse influence of earlier springs on peak summer forest greenness, actual evapotranspiration and productivity at interannual time scales across the drier western and central sections of the North American boreal forests. In the vast regions where this spring onset mechanism operates, ecosystem productivity gains from earlier springs during the early portion of the growing season are effectively cancelled through corresponding losses in the later portion. Our results also indicate that recent decadal shifts towards earlier springs and associated drying in the midst of the growing season over western North American boreal forests may have contributed to the reported declines in summer productivity and increases in tree mortality and fire activity. With projections of accelerated northern high-latitude warming and associated shifts to earlier springs, persistent soil moisture deficits in peak summer may be an effective mechanism for regional-scale boreal forest dieback through their strong influence on productivity, tree mortality and disturbance dynamics.

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Journal ArticleDOI

Seasonal Responses of Net Primary Productivity of Vegetation to Phenological Dynamics in the Loess Plateau, China

TL;DR: In this article , the authors calibrated and analyzed the normalized difference vegetation index (NDVI) time series of Advanced Very-High-Resolution Radiometer (AVHRR) data from 1982 to 2015 in the Loess Plateau, China.
Journal ArticleDOI

Diverse responses of vegetation phenology to changes in temperature and precipitation in Northern China

TL;DR: Wang et al. as mentioned in this paper analyzed the response relationship of SOS and EOS to average temperature and precipitation in each period and found that SOS, EOS, the average timing of SOS (AvSOS), and the average time of EOS (AvEOS) all had strong spatial heterogeneity.
Book ChapterDOI

Diagnosing Environmental Controls on Vegetation Greening and Browning Trends Over Alaska and Northwest Canada Using Complementary Satellite Observations

TL;DR: In this paper, the authors used satellite-derived observations of vegetation greenness (EVI), sun-induced chlorophyll fluorescence (SIF) and gross primary productivity (GPP) to clarify regional patterns and recent variations in vegetation growth over the Arctic Boreal Vulnerability Experiment (ABoVE) domain.
Journal ArticleDOI

Interactions within the climate-vegetation-fire nexus may transform 21st century boreal forests in northwestern Canada

TL;DR: This article used a dynamic global vegetation model to project annual burn rates, as well as tree species composition and biomass in Canada's Northwest Territories (NT) during the 21st century using the IPCC's climate scenarios.
Book ChapterDOI

Longer Growing Season Decreases Peak Summer Vegetation Productivity in North American Ecosystems

TL;DR: In this article, the authors analyzed the relationship between longer non-frozen period, peak summer vegetation greenness index and a drought index by using the three decades of optical satellite data, microwave Freeze-Thaw record and climatic data.
References
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Climate change 2007: the physical science basis

TL;DR: The first volume of the IPCC's Fourth Assessment Report as mentioned in this paper was published in 2007 and covers several topics including the extensive range of observations now available for the atmosphere and surface, changes in sea level, assesses the paleoclimatic perspective, climate change causes both natural and anthropogenic, and climate models for projections of global climate.
Book

Climate change 2007 : the physical science basis : contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change

Susan Solomon
TL;DR: In this article, the authors present a historical overview of climate change science, including changes in atmospheric constituents and radiative forcing, as well as changes in snow, ice, and frozen ground.
Journal ArticleDOI

A Multiscalar Drought Index Sensitive to Global Warming: The Standardized Precipitation Evapotranspiration Index

TL;DR: In this article, a new climatic drought index, the standardized precipitation evapotranspiration index (SPEI), is proposed, which combines multiscalar character with the capacity to include the effects of temperature variability on drought assessment.
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