Adaptation to climate change in the Northeast United States: opportunities, processes, constraints

2007 ◽  
Vol 13 (5-6) ◽  
pp. 643-659 ◽  
Author(s):  
Susanne C. Moser ◽  
Roger E. Kasperson ◽  
Gary Yohe ◽  
Julian Agyeman
2015 ◽  
Vol 120 (20) ◽  
pp. 10,569-10,592 ◽  
Author(s):  
Fangxing Fan ◽  
Raymond S. Bradley ◽  
Michael A. Rawlins

2017 ◽  
Vol 78 ◽  
pp. 49-57 ◽  
Author(s):  
Sarah L. Smith ◽  
Shannon E. Cunniff ◽  
Natalie S. Peyronnin ◽  
Jacob P. Kritzer

2021 ◽  
Vol 14 (1) ◽  
Author(s):  
Obste Therasme ◽  
Timothy A. Volk ◽  
Mark H. Eisenbies ◽  
Thomas E. Amidon ◽  
Marie-Odile Fortier

Abstract Background The amount of carbon dioxide in the atmosphere has been on the rise for more than a century. Bioenergy crops are seen by the Intergovernmental Panel on Climate Change as an essential part of the solution to addressing climate change. To understand the potential impact of shrub willow (Salix spp.) crop in the northeast United States, effective and transparent life cycle assessment of these systems needs to occur. Results Here we show, ethanol produced from the fermentation of sugars from hot water extract of willow grown on cropland can sequester 0.012 ± 0.003 kg CO2eq MJ−1 for a supply system incorporating summer harvest and storage. Despite decreases in soil organic carbon when willow is instead grown on grassland, the produced fuel still can provide significant climate benefits compared to gasoline. Conclusions Shrub willow converted to ethanol can be a carbon negative source of transportation fuel when the electricity and heat required for the conversion process are generated from renewable biomass. The sequestration of carbon in the belowground portion of the plants is essential for the negative GHG balance for cropland and low GHG emissions in grassland.


2007 ◽  
Vol 13 (5-6) ◽  
pp. 607-613 ◽  
Author(s):  
Lewis H. Ziska ◽  
Paul R. Epstein ◽  
Christine A. Rogers

2007 ◽  
Vol 13 (5-6) ◽  
pp. 419-423 ◽  
Author(s):  
Peter C. Frumhoff ◽  
James J. McCarthy ◽  
Jerry M. Melillo ◽  
Susanne C. Moser ◽  
Donald J. Wuebbles ◽  
...  

Author(s):  
Nima Ehsani ◽  
Charles J. Vörösmarty ◽  
Balázs M. Fekete ◽  
Eugene Z. Stakhiv

A large-scale, high-resolution, fully coupled hydrological/reservoir/hydroelectricity model is used to investigate the impacts of climate change on hydroelectricity generation and hydropower potential of non-powered dams across the Northeast United States megaregion with 11,037 dams and 375 hydroelectric power plants. The model is calibrated and validated using the U.S. Department of Energy records. Annual hydroelectricity generation in the region is 41 Terawatt-hours (Twh). Our estimate of the hydropower potential of non-powered dams adds up to 350 Twh. West Virginia, Virginia, Pennsylvania, and New York have significant potential for generating more hydroelectricity from already existing dams. On the other hand, this potential virtually does not exist for Rhode Island and Delaware and is small for New Jersey and Vermont. Climate change may reduce annual hydropower potential from non-powered dams by up to 13% and reduce current annual hydroelectricity generation by up to 8% annually. Increased rainfall in winters and earlier snowmelt in springs result in an increase in regional water availability in December through March. In other months, reduced precipitation and increased potential evapotranspiration rates combined with reduced recharge from the shift in spring snowmelt and smaller snowpack result in a decrease in availability of water and thus hydroelectricity generation. This changes call for the recalibration of dam operations and may raise conflict of interests in multipurpose dams.


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