scholarly journals Climate Change Perceptions and Observations of Agricultural Stakeholders in the Northern Great Plains

2018 ◽  
Vol 10 (5) ◽  
pp. 1687 ◽  
Author(s):  
Bruna Grimberg ◽  
Selena Ahmed ◽  
Colter Ellis ◽  
Zachariah Miller ◽  
Fabian Menalled
Keyword(s):  
Climate Change ◽  
Great Plains ◽  
Northern Great Plains ◽  
Change Perceptions

Climate change and shifting arrival date of migratory birds over a century in the northern Great Plains

2015 ◽  
Vol 127 (1) ◽  
pp. 43-51 ◽  
Author(s):  
Steven E. Travers ◽  
Bryan Marquardt ◽  
Nicole J. Zerr ◽  
James B. Finch ◽  
Mikayla J. Boche ◽  
...  
Keyword(s):  
Climate Change ◽  
Great Plains ◽  
Migratory Birds ◽  
Northern Great Plains ◽  
Arrival Date

scholarly journals Model-based scenario planning to inform climate change adaptation in the Northern Great Plains—Final report

2017 ◽  
Author(s):  
Amy J. Symstad ◽  
Brian W. Miller ◽  
Jonathan M. Friedman ◽  
Nicholas A. Fisichelli ◽  
Andrea J. Ray ◽  
...  
Keyword(s):  
Climate Change ◽  
Climate Change Adaptation ◽  
Great Plains ◽  
Scenario Planning ◽  
Northern Great Plains ◽  
Final Report ◽  
Model Based

scholarly journals Snow and albedo climate change impacts across the United States Northern Great Plains

2015 ◽  
Vol 9 (3) ◽  
pp. 3331-3349 ◽  
Author(s):  
S. R. Fassnacht ◽  
M. L. Cherry ◽  
N. B. H. Venable
Keyword(s):  
Climate Change ◽  
United States ◽  
Great Plains ◽  
Minimum Temperature ◽  
Climate Change Impacts ◽  
The United States ◽  
Snow Accumulation ◽  
Northern Great Plains ◽  
Climate Trends ◽  
Precipitation Total

Abstract. In areas with a seasonal snowpack, a warmer climate would cause less snowfall, a shallower snowpack and a change in the timing of snowmelt. Trends in temperature, precipitation (total and as snow), days with precipitation and snow, and winter albedo were investigated over the 60 year period from 1951 to 2010 for 20 meteorological stations across the Northern Great Plains. This is an area where snow accumulation is shallow but persistent for most of the winter (November through March). The most consistent trends were minimum temperature and days with precipitation, which both increased at a majority of the stations. The modeled winter albedo decreased at more stations than where it increased. There were substantial spatial variability in the climate trends. For most variables, the period of record used influenced the magnitude and sign of the significant trends.

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