Date of Award

Spring 2026

Language

English

Embargo Period

5-1-2026

Document Type

Master's Thesis

Degree Name

Master of Science (MS)

College/School/Department

Department of Atmospheric and Environmental Sciences

Program

Atmospheric Science

First Advisor

Aiguo Dai

Committee Members

Aiguo Dai, Justin Minder

Keywords

Climate, Precipitation, Climatology, Climate Change, Climate Science, Radar

Subject Categories

Atmospheric Sciences

Abstract

As anthropogenic greenhouse gas emissions continue to warm the global climate system, improving our understanding of how precipitating storms are responding in the real world has become increasingly important.  This study leverages 22 years of high-resolution hourly precipitation data from the NCEP Stage IV dataset to produce a seasonal climatology and long-term trend analysis of precipitating storm frequency, duration, area, and intensity across the Contiguous United States (CONUS) from March 2002 through February 2024.  Storms were identified and tracked using an object-tracking algorithm and their characteristics were computed for each season, from which 22-year climatology and trends were derived.  The storm climatology is dominated by a pronounced east-west contrast in all storm properties across all seasons, with the eastern half of CONUS supporting substantially more active storm environments than the western half, driven by synoptic storm tracks and abundant moisture. The Gulf Coast and Southeast stand out as CONUS’s most intense storm regions across all seasons.  Long-term trend analysis reveals a counterintuitive but physically coherent picture: storms over CONUS are simultaneously growing larger and lasting longer across all seasons yet delivering progressively weaker intensities at many locations, which is inconsistent with model-projected response to global warming. Storm formation frequency is declining during summer and fall, while winter storms have become modestly more common, which is consistent with model projected changes. These trends collectively suggest a broad structural transition in CONUS storm characteristics away from intense, discrete convective systems and towards more expansive and long-lived storm systems. This shift carries significant implications for severe weather risk, water resource availability, and regional precipitation distribution across CONUS.

License

Creative Commons Attribution 4.0 International License
This work is licensed under a Creative Commons Attribution 4.0 International License.

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