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Weather modeling

Modeling project

Inside an Appalachian extreme-rainfall event

Using nested WRF simulations and Stage IV precipitation to study the July 2022 Central Appalachian flood event.

Pinkrah Nana Ofosuhene

Model
WRF / WPS
Forcing
ERA5
Event
26–27 July 2022
Verification
Stage IV

The question

How well can a regional weather model represent an extreme-rainfall event?

This numerical weather prediction project examines the evolution and spatial organization of precipitation during the July 2022 Central Appalachian flood event.

Data & methods

A closer look at
the approach.

The workflow combines WRF preprocessing, ERA5 initial and boundary conditions, nested-domain simulation, precipitation accumulation, and comparison with Stage IV precipitation.

Findings & context

What the work shows.

  • Six-hour accumulation maps track the movement and concentration of simulated precipitation.
  • Verification against Stage IV examines the location and magnitude of modeled rainfall.
  • The case study complements statistical climate analysis with a process-based view of an individual high-impact event.

Research and coursework simulation; not an operational forecast.

From the analysis

Research figures.

Select a figure to view it larger.

Simulated precipitation accumulation, 00–06 UTC on 26 July 2022.
FIG. 01Simulated precipitation accumulation, 00–06 UTC on 26 July 2022.
Simulated precipitation accumulation, 06–12 UTC on 26 July 2022.
FIG. 02Simulated precipitation accumulation, 06–12 UTC on 26 July 2022.
Simulated precipitation accumulation, 18 UTC 26 July–00 UTC 27 July 2022.
FIG. 03Simulated precipitation accumulation, 18 UTC 26 July–00 UTC 27 July 2022.
WRF precipitation verification against Stage IV precipitation.
FIG. 04WRF precipitation verification against Stage IV precipitation.

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Research figure