LanguageTerm (authority = ISO 639-3:2007); (type = text)
English
Abstract (type = abstract)
This dissertation develops a climatology of water vapor fluxes for the eastern United States and investigates its relationship with precipitation. This approach enriches the current literature, which relates changes in precipitation in the eastern US to weather patterns but largely overlooks the role of moisture supply. Because atmospheric water vapor content is sensitive to temperature, this dissertation contributes new knowledge on how large-scale climate variability impacts regional precipitation. This knowledge is foundational for interpreting past, present, and projected changes in precipitation and understanding its impacts in regional climatology and water resources applications.
Major patterns of water vapor transport in the eastern US are identified using a self-organizing map methodology ingesting daily moisture fluxes from the European Centre for Medium-Range Weather Forecasts (ECMWF) ERA-Interim reanalysis from 1979–2017 for 30°–50°N × 60°–90°W. This procedure produces sixteen patterns of integrated water vapor transport (IVT) that encompass the variety of moisture transport through the region. Spatial and temporal characteristics of these patterns, including moisture distribution across the domain, qualities of atmospheric rivers, frequency, seasonality, and persistence of the patterns are examined. This resulting climatology presents a precise and comprehensive framework for relating atmospheric moisture supply to precipitation.
This climatology is related to precipitation from 1981–2017 using PRISM daily precipitation data and is extended to 1900–2010 using empirical precipitation data and ECMWF ERA-20C IVT reanalysis. These relationships reveal that the semi-frequent patterns defined by moderate moisture transport are important contributors to annual precipitation, and that the majority of moisture transport patterns are associated with increasing amounts of heavy precipitation. Additionally, increases in the frequency and intensity of strong, meridional moisture transport patterns result in changes in the moisture patterns most often associated with heavy precipitation in the eastern US. These results demonstrate the sensitivity of the eastern US precipitation regime to variability in moisture transport, indicating a need for future studies of regional precipitation to include this information. Overall, this study of kinematic moisture transport provides a new framework for better understanding precipitation variability.
Subject (authority = local)
Topic
Climatology
Subject (authority = RUETD)
Topic
Geography
RelatedItem (type = host)
TitleInfo
Title
Rutgers University Electronic Theses and Dissertations
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