U. COLORADO—As the climate warms and growing seasons lengthen, subalpine forests are likely to soak up less carbon dioxide. The result will be more greenhouse gas left to concentrate in the atmosphere, new research shows.
“Our findings contradict studies of other ecosystems that conclude longer growing seasons actually increase plant carbon uptake,” says Jia Hu, who conducted the research as a graduate student in the ecology and evolutionary biology department at University of Colorado at Boulder, in conjunction with the Cooperative Institute for Research in Environmental Sciences (CIRES).
The study will be published in the February edition of the journal Global Change Biology.
Working with ecology and evolutionary biology professor and CIRES fellow Russell Monson, Hu found that while smaller spring snowpack tended to advance the onset of spring and extend the growing season, it also reduced the amount of water available to forests later in the summer and fall.
The water-stressed trees were then less effective in converting CO2 into biomass. Summer rains were unable to make up the difference, Hu says.
“Snow is much more effective than rain in delivering water to these forests,” explains Monson. “If a warmer climate brings more rain, this won’t offset the carbon uptake potential being lost due to declining snowpacks.”
Drier trees also are more susceptible to beetle infestations and wildfires, Monson continues.
Even as late in the season as September and October, 60 percent of the water in stems and needles collected from subalpine trees along Colorado’s Front Range can still be traced back to spring snowmelt.
The researchers were able to distinguish between spring snow and summer rain in plant matter by analyzing slight variations in hydrogen and oxygen atoms in the water molecules.
The results suggest subalpine trees like lodgepole pine, subalpine fir and Englemann spruce depend largely on snowmelt, not just at the beginning of the summer, but throughout the growing season, according to the researchers.
“As snowmelt in these high-elevation forests is predicted to decline, the rate of carbon uptake will likely follow suit,” predicts Hu.
Subalpine forests currently make up an estimated 70 percent of the western United States’ carbon sink, or storage area.
Their geographic range includes much of the Rocky Mountains, Sierra Nevada, and high-elevation areas of the Pacific Northwest.
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