A Hybrid Dataset of Historical Cool-Season Lake Effects From the Eastern Great Lakes of North America
dc.contributor.author | Ellis, Andrew W. | en |
dc.contributor.author | Suriano, Zachary J. | en |
dc.date.accessioned | 2022-07-25T13:30:05Z | en |
dc.date.available | 2022-07-25T13:30:05Z | en |
dc.date.issued | 2022-02-21 | en |
dc.description.abstract | The moistening of cold air passing over the Great Lakes of North America has a profound impact on the cool season climate of regions downwind, from relatively benign air mass modification to highly-impactful snowfall events. The importance of lake effects has led to the development of varying techniques for systematically identifying lake-effect days. The results of two such methods are merged here to yield a more thorough record of lake-effect days for the eastern Great Lakes. Comparative analysis of the data sets illustrates the different objectives of the two methodologies, where one identifies days with a synoptic setup conducive to lake-effect snowfall, and the other identifies days with lake-effect modification of the overlying air mass. A smaller population of "absolute" lake-effect days are those identified by both methods, while a larger population of "hybrid" lake-effect days are absolute days plus those identified by one method but not the other. For a 51-year study period ending with the 2014-15 cool season, the absolute data set yields a mean of about 15 lake-effect days per year, or 8% of the November through April season, while the hybrid data set yields a mean of 56 lake-effect days per year, or 31% of the season. The frequencies of absolute, air mass modification-defined, and hybrid lake-effect days decreased through the study period, with days within the hybrid data set declining at a statistically significant rate of 2.8 days per decade, although most obviously from the late 1970s through the early 2000s. The result is a general drying of the cool-season lake-effect hydroclimate. The merged data set offers a more thorough historical record of days available for atmospheric and hydroclimatic study of the lake-effect phenomenon within the eastern Great Lakes region. | en |
dc.description.version | Published version | en |
dc.format.mimetype | application/pdf | en |
dc.identifier.doi | https://doi.org/10.3389/frwa.2022.788493 | en |
dc.identifier.eissn | 2624-9375 | en |
dc.identifier.other | 788493 | en |
dc.identifier.uri | http://hdl.handle.net/10919/111350 | en |
dc.identifier.volume | 4 | en |
dc.language.iso | en | en |
dc.publisher | Frontiers | en |
dc.rights | Creative Commons Attribution 4.0 International | en |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/ | en |
dc.subject | Great Lakes | en |
dc.subject | lake-effect | en |
dc.subject | cool season | en |
dc.subject | Synoptic Classification | en |
dc.subject | hydroclimate | en |
dc.title | A Hybrid Dataset of Historical Cool-Season Lake Effects From the Eastern Great Lakes of North America | en |
dc.title.serial | Frontiers in Water | en |
dc.type | Article - Refereed | en |
dc.type.dcmitype | Text | en |
Files
Original bundle
1 - 1 of 1
Loading...
- Name:
- frwa-04-788493.pdf
- Size:
- 3.36 MB
- Format:
- Adobe Portable Document Format
- Description:
- Published version