Datasets

creator: Daniel Robert Chavas, 0000-0001-9172-8328 date: 2023

Total is 4 Results
Chavas and Peters (2023, BAMS): Static energy deserves greater emphasis in the meteorology community.

10.4231/TJK1-HS57

Daniel Robert Chavas ORCID logo , John Peters

10/26/2023

Excel file for Figure 1 and MATLAB code + data for Figures 2 and 3 of the manuscript Chavas and Peters (2023) accepted for publication in Bulletin of the American Meteorological Society

Climate Education potential temperature static energy Weather

Dataset/Codes for the project: A Model for the Tropical Cyclone Wind Field Response to Idealized Landfall

10.4231/3AKW-VX52

Daniel Robert Chavas ORCID logo , Jie Chen ORCID logo

04/03/2023

This dataset provides the CM1 scripts to reproduce the idealized TC landfalls, and simulation outputs of the landfall experiments examined in the paper.

EAPS Hurricanes TC hazards TC landfalls TC structure theoretical TC wind field model tropical cyclones

Chavas and Peters (2023, BAMS): Static energy has important conceptual benefits for explaining how our atmosphere works.

10.4231/5DVH-KV88

Daniel Robert Chavas ORCID logo , John Peters

04/13/2023

Excel file for Figure 1 and MATLAB code + data for Figures 2 and 3 of the manuscript Chavas and Peters (2023) submitted to Bulletin of the American Meteorological Society

Climate energy Entropy potential temperature static energy teaching thermodynamics Weather

SST profiles and CESM2 model builds for "Westward extension of the Western North Pacific subtropical high forced by sea surface temperature anomaly patterns"

10.4231/R2HS-B771

Daniel Robert Chavas ORCID logo , Jhordanne Jones ORCID logo , Zachary Freitag Johnson ORCID logo

01/25/2023

Archived model builds and original sea surface temperature (SST) forcing files for simulations used in the manuscript, "Westward extension of the Western North Pacific subtropical high forced by sea surface temperature anomaly patterns".

CAM6 CESM2 Climate Variability EAPS ERA5 Global Climate Models Reanalysis Simulations Subtropical Highs

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