UNH Research: Longer Mud Season, No Snow Could Alter Northeast Rivers by 2100

DURHAM, N.H. – As temperatures begin to drop and fall transitions into winter, snow will soon blanket the northern regions of the United States. But researchers at the University of New Hampshire have found that snow cover is on the decline in this area due to climate change and the shift from winter to spring, known as the vernal window, is getting longer.

UNH Digs Deep Testing Wastewater for Early Warning Signs of COVID-19

DURHAM, N.H.— The University of New Hampshire has gone underground to flush out cases of the coronavirus by testing wastewater on campus. The sewage sampling is being used as a secondary surveillance method to the already required twice a week individual nasal test to track and detect SARS-CoV-2, the virus that causes COVID-19.

UNH Scientist Finds 2020 Severe Drought Likely to Slow Tree Growth Next Year

DURHAM, N.H.—Red oak and white pine trees could experience slower growth next year as a result of the severe drought in New Hampshire and most of New England that began in mid-August, according to a researcher with the New Hampshire Agricultural Experiment Station at the University of New Hampshire.

UNH Receives Grant to Enhance Energy and Water Needs on Coastal Islands

DURHAM, N.H.— Living on a remote island can be idyllic but it does come with some challenges when accessing inexpensive and reliable energy as well as clean drinking water. The University of New Hampshire has received a grant from the U.S. Economic Development Agency to help island communities in the Gulf of Maine find viable and sustainable solutions modeled after a renewable energy microgrid system that powers the Shoals Marine Laboratory (SML) on Appledore Island.

UNH Receives NSF Grant to Research Carbon Interactions in Thawing Arctic

DURHAM, N.H.— The University of New Hampshire will lead research as part of a $1.5 million award from the National Science Foundation (NSF) to better understand how interactions between plants, microbes and soil minerals in permafrost, a subsurface layer of frozen soil covering a fourth of the Northern Hemisphere, stimulate the release of carbon which adds to the warming Arctic.