Analytical Model for the Higher Order Moments of Midlatitude Atmospheric Temperature Distributions

Abstract Observed distributions of atmospheric temperature are non‐Gaussian. Therefore, moments beyond variance are necessary in determining the frequency of extreme temperature events. Here we propose a simple kinematic model for atmospheric mid‐latitude temperature variability based on symmetric advection from a non‐symmetric background temperature profile. We then use this model to derive analytical expressions for the higher order moments of temperature distributions. Our results show that nonzero skewness and kurtosis arise due to the nonlinearity of the time‐mean meridional temperature profile. The analytical model matches an idealized Held‐Suarez atmospheric model, indicating nonlinearity of time‐mean temperature in latitude is the dominant contribution to nonzero skewness and kurtosis in synoptic temperature variations. Model analysis further shows decrease in higher order moments due to climate change come roughly equally from changes in mixing length and changes in the background temperature profiles.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-02-05
DOI
https://doi.org/10.1029/2024gl111626
Citations
1
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
1.11

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article

Analytical Model for the Higher Order Moments of Midlatitude Atmospheric Temperature Distributions

Cristian Proistosescu, Ryan L. Sriver, Keiko Ino Kircher
1 citations
Geophysical Research Letters
Climate variability and models
1.11
article

Analytical Model for the Higher Order Moments of Midlatitude Atmospheric Temperature Distributions

Cristian Proistosescu, Ryan L. Sriver, Keiko Ino Kircher
article en
1 citations

Abstract

Abstract Observed distributions of atmospheric temperature are non‐Gaussian. Therefore, moments beyond variance are necessary in determining the frequency of extreme temperature events. Here we propose a simple kinematic model for atmospheric mid‐latitude temperature variability based on symmetric advection from a non‐symmetric background temperature profile. We then use this model to derive analytical expressions for the higher order moments of temperature distributions. Our results show that nonzero skewness and kurtosis arise due to the nonlinearity of the time‐mean meridional temperature profile. The analytical model matches an idealized Held‐Suarez atmospheric model, indicating nonlinearity of time‐mean temperature in latitude is the dominant contribution to nonzero skewness and kurtosis in synoptic temperature variations. Model analysis further shows decrease in higher order moments due to climate change come roughly equally from changes in mixing length and changes in the background temperature profiles.

Geophysical Research LettersVol. 52(3)
University of Illinois Urbana-Champaign (US)
U.S. Department of Energy
Climate action
Openalex Percentile: Top 28%
Climate variability and models
1.11
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