The PIRLA project (paleoecological investigation of recent lake acidification): Preliminary results for the Adirondacks, New England, N. Great Lakes states, and N. Florida

1986 ◽  
Vol 30 (1-2) ◽  
pp. 355-365 ◽  
Author(s):  
Donald F. Charles ◽  
Donald R. Whitehead ◽  
Dennis S. Anderson ◽  
Raymond Bienert ◽  
Keith E. Camburn ◽  
...  
1986 ◽  
pp. 355-365
Author(s):  
Donald F. Charles ◽  
Donald R. Whitehead ◽  
Dennis S. Anderson ◽  
Raymond Bienert ◽  
Keith E. Camburn ◽  
...  

1990 ◽  
Vol 4 (2) ◽  
pp. 153-201 ◽  
Author(s):  
J. C. Kingston ◽  
R. B. Cook ◽  
R. G. Kreis ◽  
K. E. Camburn ◽  
S. A. Norton ◽  
...  

2021 ◽  
Vol 13 (4) ◽  
pp. 1677
Author(s):  
Emma Uebelhor ◽  
Olivia Hintz ◽  
Sarah B. Mills ◽  
Abigail Randall

In the coming years, it is expected that reliance on utility-scale solar projects for energy production will increase exponentially. As a result, communities throughout the Midwest will become potential solar facility hosts. Previous research has sought to identify factors that influence community support and opposition to solar developments throughout the country. This paper builds upon prior research by examining community perceptions about the economic, environmental, local and global impact of solar projects in four Great Lakes states using a content analysis of local newspaper articles. Ultimately, this paper identifies the most common perceptions of solar facilities and offers some preliminary suggestions on strategies to mitigate the most prevalent concerns.


Author(s):  
Janel Hanrahan ◽  
Jessica Langlois ◽  
Lauren Cornell ◽  
Huanping Huang ◽  
Jonathan Winter ◽  
...  

AbstractMost inland water bodies are not resolved by General Circulation Models, requiring that lake surface temperatures be estimated. Given the large spatial and temporal variability of the North American Great Lakes’ surface temperatures, such estimations can introduce errors when used as lower boundary conditions for dynamical downscaling. Lake surface temperatures (LSTs) influence moisture and heat fluxes, thus impacting precipitation within the immediate region and potentially in regions downwind of the lakes. For the present study, the Advanced Research Weather Research and Forecasting Model (WRF-ARW) was used to simulate precipitation over six New England states during a five-year historical period. The model simulation was repeated with perturbed LSTs, ranging from 10°C below to 10°C above baseline values obtained from reanalysis data, to determine whether the inclusion of erroneous LST values impact simulated precipitation and synoptic-scale features. Results show that simulated precipitation in New England is statistically correlated with LST perturbations, but this region falls on a wet-dry line of a larger bimodal distribution. Wetter conditions occur to the north and drier conditions to the south with increasing LSTs, particularly during the warm season. The precipitation differences coincide with large-scale anomalous temperature, pressure, and moisture patterns. Care must therefore be taken to ensure reasonably accurate Great Lakes’ surface temperatures when simulating precipitation, especially in southeastern Canada, Maine, and the Mid-Atlantic region.


2018 ◽  
Vol 62 (6) ◽  
pp. 1089-1107 ◽  
Author(s):  
Mark J. Ducey ◽  
Kenneth M. Johnson ◽  
Ethan P. Belair ◽  
Barbara D. Cook

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