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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

The chained effects of earlier vegetation activities and summer droughts on ecosystem productivity on the Tibetan Plateau

TL;DR: In this article , Wang et al. evaluated the chained effects between earlier vegetation activities and summer droughts on the Tibetan Plateau (TP) and found that higher spring vegetation productivity is caused by early vegetation activities, partially compensated for summer drought-induced loss.

Seasonal differences in the relationships between the changes in spring phenology and the dynamics of carbon cycle for grasslands

Z. Xie, +2 more
TL;DR: In this article, the authors investigated the relationship between spring phenological changes and the dynamics of carbon cycle, including NEP; ecosystem respiration, ER; and gross ecosystem production, at a ten-day scale.
Book ChapterDOI

Spring Phenology of the Boreal Ecosystems

TL;DR: In this article, a remote sensing green-up retrieval method designed to avoid signal contamination by snow was presented, and the result validation with ground observations showed that the method caught the interannual variations in phenology of the plant community.
Posted ContentDOI

Increasing summer net CO 2 uptake in high northern ecosystems inferred from atmospheric inversions and remote sensing

TL;DR: In this paper, the authors examine CO2 fluxes from northern boreal and tundra from 1986 to 2012 estimated from two inverse models (RIGC and Jena), both using measured atmospheric CO2 concentrations and wind-fields from interannually variable reanalysis.
Journal ArticleDOI

Vegetation Productivity Losses Linked to Mediterranean Hot and Dry Events

TL;DR: In this article, the productivity of Mediterranean vegetation is affected by hot and dry events, examining a set of severe episodes that occurred in three different regions (Iberian Peninsula, Eastern Mediterranean and Western Europe) between 2001 and 2019.
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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