{"title":"Cool season near-surface wind speed trends across the central Appalachian Mountains region of the eastern United States, 1995-2022","authors":"Andrew W. Ellis","doi":"10.1080/02723646.2023.2275815","DOIUrl":null,"url":null,"abstract":"ABSTRACTPrompted by recent findings of a common trend toward lesser near-surface winds (NSW), or stilling, time series of cool season NSW variables for 20 stations in the central Appalachian Mountains of the eastern United States were examined for trends during the period 1995–2022. While not universal across the station array, results generally indicate an increase in the frequency of calm conditions, a decrease in mean wind velocity, and a decrease in the frequency of high-wind days. Contrasting this was a general increase in high-wind gust days. The evidence for stilling was supported by an increase in the frequency of days with a 12-hour pressure change of zero and an apparent strengthening and northwestward expansion of the subtropical ridge over the region. Supporting the increase in high-wind gust days was an increase in the frequency of days with a large 3-hour pressure change, and lesser geopotential heights in the lower atmosphere northwest of the region, which contrasts the expanding subtropical ridge and together presents the potential for periodic placement of stronger dynamics across the region.KEYWORDS: Near-surface windAppalachian mountainsstilling AcknowledgmentsThe author thanks Mr. Jacob Feurer for assistance with data preparation, Mr. Ryan Holgerson for providing editorial comments, and two anonymous reviewers for significant guidance that improved the manuscript greatly.Disclosure statementNo potential conflict of interest was reported by the author(s).Data availability statementMETAR wind data are available from the Iowa Environmental Mesonet (IEM) data archive at Iowa State University https://mesonet.agron.iastate.edu/request/download.phtml and the Integrated Surface Database of the United States National Centers for Environmental Information (https://www.ncei.noaa.gov/access/search/data-search/global-hourly). United States National Center for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis data are available at https://psl.noaa.gov/cgi-bin/data/composites/printpage.pl. Alternately, the distilled data used in the study can be obtained from the author (awellis@vt.edu).","PeriodicalId":54618,"journal":{"name":"Physical Geography","volume":"159 6","pages":"0"},"PeriodicalIF":1.1000,"publicationDate":"2023-10-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physical Geography","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/02723646.2023.2275815","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
ABSTRACTPrompted by recent findings of a common trend toward lesser near-surface winds (NSW), or stilling, time series of cool season NSW variables for 20 stations in the central Appalachian Mountains of the eastern United States were examined for trends during the period 1995–2022. While not universal across the station array, results generally indicate an increase in the frequency of calm conditions, a decrease in mean wind velocity, and a decrease in the frequency of high-wind days. Contrasting this was a general increase in high-wind gust days. The evidence for stilling was supported by an increase in the frequency of days with a 12-hour pressure change of zero and an apparent strengthening and northwestward expansion of the subtropical ridge over the region. Supporting the increase in high-wind gust days was an increase in the frequency of days with a large 3-hour pressure change, and lesser geopotential heights in the lower atmosphere northwest of the region, which contrasts the expanding subtropical ridge and together presents the potential for periodic placement of stronger dynamics across the region.KEYWORDS: Near-surface windAppalachian mountainsstilling AcknowledgmentsThe author thanks Mr. Jacob Feurer for assistance with data preparation, Mr. Ryan Holgerson for providing editorial comments, and two anonymous reviewers for significant guidance that improved the manuscript greatly.Disclosure statementNo potential conflict of interest was reported by the author(s).Data availability statementMETAR wind data are available from the Iowa Environmental Mesonet (IEM) data archive at Iowa State University https://mesonet.agron.iastate.edu/request/download.phtml and the Integrated Surface Database of the United States National Centers for Environmental Information (https://www.ncei.noaa.gov/access/search/data-search/global-hourly). United States National Center for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis data are available at https://psl.noaa.gov/cgi-bin/data/composites/printpage.pl. Alternately, the distilled data used in the study can be obtained from the author (awellis@vt.edu).
期刊介绍:
Physical Geography disseminates significant research in the environmental sciences, including research that integrates environmental processes and human activities. It publishes original papers devoted to research in climatology, geomorphology, hydrology, biogeography, soil science, human-environment interactions, and research methods in physical geography, and welcomes original contributions on topics at the intersection of two or more of these categories.