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1. A geography of lake carbon cycling: Geography of lake carbon cycling

   https://doi.org/10.1002/lol2.10078  

   Seekell, David A.; Lapierre, Jean-François; Cheruvelil, Kendra Spence (June 2018, Limnology and Oceanography Letters)
2. A Climatology of Easterly Wind Lake-Effect and Lake-Enhanced Precipitation Events over the Western Lake Superior Region

   https://doi.org/10.1175/JAMC-D-22-0080.1  

   Sandstrom, Joshua D.; Cordeira, Jason M.; Hoffman, Eric G.; Metz, Nicholas D. (February 2023, Journal of Applied Meteorology and Climatology)

   Abstract Lake-effect precipitation is convective precipitation produced by relatively cold air passing over large and relatively warm bodies of water. This phenomenon most often occurs in North America over the southern and eastern shores of the Great Lakes, where high annual snowfalls and high-impact snowstorms frequently occur under prevailing west and northwest flow. Locally higher snow or rainfall amounts also occur due to lake-enhanced synoptic precipitation when conditionally unstable or neutrally stratified air is present in the lower troposphere. While likely less common, lake-effect and lake-enhanced precipitation can also occur with easterly winds, impacting the western shores of the Great Lakes. This study describes a 15-year climatology of easterly lake-effect (ELEfP) and lake-enhanced (ELEnP) precipitation (conjointly Easterly Lake Collective Precipitation: ELCP) events that developed in east-to-east-northeasterly flow over western Lake Superior from 2003 to 2018. ELCP occurs infrequently but often enough to have a notable climatological impact over western Lake Superior with an average of 14.6 events per year. The morphology favors both single shore-parallel ELEfP bands due to the convex western shoreline of Lake Superior and mixed-type banding due to ELEnP events occurring in association with “overrunning” synoptic-scale precipitation. ELEfP often occurs in association with a surface anticyclone to the north of Lake Superior. ELEnP typically features a similar northerly-displaced anticyclone and a surface cyclone located over the U.S. Upper Midwest that favor easterly boundary-layer winds over western Lake Superior. 

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3. What Is in a “Lake” Name? That Which We Call a Lake by Any Other Name

   https://doi.org/10.1002/lob.10355  

   Soranno, Patricia A.; Webster, Katherine E.; Smith, Nicole J.; Díaz Vázquez, Jessica; Cheruvelil, Kendra Spence (February 2020, Limnology and Oceanography Bulletin)

   Abstract Given how important lakes are to people, it might seem safe to assume that careful thought has been put into the naming of lakes, and that lake names reflect the high societal value people place on lakes. We examined these assumptions by analyzing the official names in the U.S. Geographic Names Information System for the 479,950 lakes ≥ 1 ha in the conterminous U.S. We found that 83% of lakes were unnamed and most of these were small lakes with 80% of unnamed lakes being smaller than 4 ha. Based on the 83,115 named lakes, we found that lake names reflect peoples' everyday lives, that lakes can inspire creativity (although the most common lake name is “Mud”), that Native American and indigenous languages have played a role in lake naming, and that there are regional differences in lake names. Unfortunately, we also found that derogatory terms were part of some lake names. We advocate for thoughtful and inclusive official naming of the 400,000 unnamed lakes in the U.S., as well as renaming of the lakes with derogatory terms to help focus attention on the importance of lakes to local communities and nations. 

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4. TOWARDS A COMPREHENSIVE ANALYSIS OF LATE-GLACIAL LAKE LEVELS WITHIN THE LAKE SUPERIOR BASIN

   https://doi.org/10.1130/abs/2025NE-408499  

   Pellegrino, Jay; Breckenridge, Andy; Wieker, Matt (March 2025, 2025 Joint Northeastern and North-Central Section Meeting)

   The increasing availability of LiDAR digital elevation models (DEMs) for Canada and the United States is improving our ability to recognize and detail the geomorphological record of former glacial lakes revealed by strandlines. More accurate strandline maps refine our understanding of glacial-isostatic adjustment (GIA), reveal information about deglacial ice margins, help identify rapid drawdown events and catastrophic flooding by ice dam failure, and advance models that connect waterplane curvature to age. Here we present new strandline maps in the Lake Superior Basin based on LiDAR DEMs from Wisconsin, Michigan, and Ontario. When combined with published records from Minnesota, they comprise the most extensive set of strandlines detailing former lake levels from any lake basin. Multiple lakes and lake phases are associated with these strandlines, including glacial lakes Wrenshall, Ontonagon, Duluth, Algonquin and Minong, as well as Holocene Lake Nipissing. The relative degree of strandline development varies widely, likely due to factors such as the availability of gravel and sand, length of time of formation, fetch, and local shoreline geometry (e.g. bay or headland). Strandlines for at least one level of glacial Lake Duluth are much more extensive on the southern shore, suggesting formation from only a very few numbers of storms with winds from the north. New LiDAR DEMs from the Sault Ste. Marie region are particularly helpful because they allow us to determine isobases (lines of equal GIA) across the primary basin outlet with high confidence. In general, our work supports the work of prior researchers, but adds details that are easily missed by field surveys or when using coarser resolution DEMs. 

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5. Lake Atitlan: A Review of the Food, Energy, and Water Sustainability of a Mountain Lake in Guatemala

   https://doi.org/10.3390/su13020515  

   Neher, Timothy P.; Soupir, Michelle L.; Kanwar, Rameshwar S. (January 2021, Sustainability)

   null (Ed.)

   This paper summarizes the findings of an extensive review of literature that was conducted to understand the historical state of the food, energy, and water nexus in the Lake Atitlan basin and to recommend incentive-based, long-term sustainable policies to become a significant driver to Guatemala’s tourism industry and GDP growth. The SWAT (Soil and Water Assessment Tool) was implemented in the basin to work towards the goal of simulating nutrient loading. A key conclusion of this review study is for the local population to have advocacy for the “zero wastewater discharge to Lake Atitlan” initiative to bring long-term benefits to lake water quality. One of the recommended policy decisions is to seek external financing from international agencies like the World Bank at low-cost interest (IDA Loans) to implement waste management systems and pay this external debt by putting a small but affordable tax on tourists visiting the lake. Once a culture of zero municipal effluent discharge to Lake Atitlan is adopted by the local population, the livelihood of residents will become sustainable and the standard of living will increase because of improved water and air quality, making Lake Atitlan a haven of tourism for Guatemala and lifting its economy. 

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