The nonnormality of temperature probability distributions and the physics that drive it are important due to their relationships to the frequency of extreme warm and cold events. Here we use a conditional mean framework to explore how horizontal temperature advection and other physical processes work together to control the shape of daily temperature distributions during 1979–2019 in the ERA5 dataset for both JJA and DJF. We demonstrate that the temperature distribution in the middle and high latitudes can largely be linearly explained by the conditional mean horizontal temperature advection with the simple treatment of other processes as a Newtonian relaxation with a spatially variant relaxation time scale and equilibrium temperature. We analyze the role of different transient and stationary components of the horizontal temperature advection in affecting the shape of temperature distributions. The anomalous advection of the stationary temperature gradient has a dominant effect in influencing temperature variance, while both that term and the covariance between anomalous wind and anomalous temperature have significant effects on temperature skewness. While this simple method works well over most of the ocean, the advection–temperature relationship is more complicated over land. We classify land regions with different advection–temperature relationships under our framework, and findmore »
Exploring the effects of temperature on intrinsic permeability and void ratio alteration through temperature-controlled experiments
- Award ID(s):
- 1804822
- Publication Date:
- NSF-PAR ID:
- 10281654
- Journal Name:
- Engineering Geology
- Volume:
- 293
- Issue:
- C
- Page Range or eLocation-ID:
- 106299
- ISSN:
- 0013-7952
- Sponsoring Org:
- National Science Foundation
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