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Using the Moist Static Energy Varian...
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Starr, Jarrett,
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Using the Moist Static Energy Variance Budget to Evaluate Tropical Cyclones in Climate Models Against Reanalyses and Satellite Observations: Model Resolution, Ocean Coupling, and Cloud Interactions /
Record Type:
Electronic resources : Monograph/item
Title/Author:
Using the Moist Static Energy Variance Budget to Evaluate Tropical Cyclones in Climate Models Against Reanalyses and Satellite Observations: Model Resolution, Ocean Coupling, and Cloud Interactions // Jarrett Starr.
Author:
Starr, Jarrett,
Description:
1 electronic resource (99 pages)
Notes:
Source: Masters Abstracts International, Volume: 85-12.
Contained By:
Masters Abstracts International85-12.
Subject:
Meteorology. -
Online resource:
https://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=30995681
ISBN:
9798382778525
Using the Moist Static Energy Variance Budget to Evaluate Tropical Cyclones in Climate Models Against Reanalyses and Satellite Observations: Model Resolution, Ocean Coupling, and Cloud Interactions /
Starr, Jarrett,
Using the Moist Static Energy Variance Budget to Evaluate Tropical Cyclones in Climate Models Against Reanalyses and Satellite Observations: Model Resolution, Ocean Coupling, and Cloud Interactions /
Jarrett Starr. - 1 electronic resource (99 pages)
Source: Masters Abstracts International, Volume: 85-12.
Tropical cyclones (TCs) are observed in general circulation models (GCMs) as well as reanalyses. However, it is known that GCMs and reanalyses struggle to accurately represent TCs and have biases in the TC frequency and intensity distributions. By employing the column-integrated moist static energy (MSE) variance budget as a process-oriented diagnostic, we can analyze the model representation of physical processes that help or hinder the development of TCs. Specifically, we analyze the radiative and surface flux feedback terms within the MSE variance budget across 5 different reanalysis datasets and 19 different GCM simulations. Binning and compositing of TC snapshots by maximum velocity and minimum mean sea level pressure allows for comparison across the GCMs and reanalyses of the feedbacks at a given intensity, as well as an examination of how the feedbacks vary with storm intensity. We find that the surface flux feedback on TC development is weaker in coupled models. Across all models, the longwave radiative feedback positively contributes to TC development and is driven by cloud effects. Models differ regarding the role of the shortwave radiative feedback, though it is generally smaller than the longwave. Regarding the intermodel spread in surface flux and radiative feedbacks at a given intensity, models with coarse resolution differ more from each other and from reanalyses than those with high resolution. These results can help us understand how differences in model representation of physical processes lead to model differences in TC intensity.
English
ISBN: 9798382778525Subjects--Topical Terms:
542822
Meteorology.
Subjects--Index Terms:
Tropical cyclones
Using the Moist Static Energy Variance Budget to Evaluate Tropical Cyclones in Climate Models Against Reanalyses and Satellite Observations: Model Resolution, Ocean Coupling, and Cloud Interactions /
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Tropical cyclones (TCs) are observed in general circulation models (GCMs) as well as reanalyses. However, it is known that GCMs and reanalyses struggle to accurately represent TCs and have biases in the TC frequency and intensity distributions. By employing the column-integrated moist static energy (MSE) variance budget as a process-oriented diagnostic, we can analyze the model representation of physical processes that help or hinder the development of TCs. Specifically, we analyze the radiative and surface flux feedback terms within the MSE variance budget across 5 different reanalysis datasets and 19 different GCM simulations. Binning and compositing of TC snapshots by maximum velocity and minimum mean sea level pressure allows for comparison across the GCMs and reanalyses of the feedbacks at a given intensity, as well as an examination of how the feedbacks vary with storm intensity. We find that the surface flux feedback on TC development is weaker in coupled models. Across all models, the longwave radiative feedback positively contributes to TC development and is driven by cloud effects. Models differ regarding the role of the shortwave radiative feedback, though it is generally smaller than the longwave. Regarding the intermodel spread in surface flux and radiative feedbacks at a given intensity, models with coarse resolution differ more from each other and from reanalyses than those with high resolution. These results can help us understand how differences in model representation of physical processes lead to model differences in TC intensity.
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https://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=30995681
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