Abstract
Freshwater has been shown to have a maximum density at about four degrees Celsius, and this leads to a phenomenon known as cabbeling. Cabbeling occurs when masses of water on different sides of the temperature of maximum density mix and create a denser mass. What happens when intruding and ambient temperatures in a gravity current are on opposite sides of the temperature of maximum density? How does cabbeling affect the evolution characteristics of gravity currents, and what sort of long term behavior arises?- Cite:
- Andrew Grace, Marek Stastna, Kevin G. Lamb, and K. Andrea Scott. 2023. Gravity currents in the cabbeling regime. Physical Review Fluids, Volume 8, Issue 1, 8(1).
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@article{Grace-2023-Gravity,
title = "Gravity currents in the cabbeling regime",
author = "Grace, Andrew and
Stastna, Marek and
Lamb, Kevin G. and
Scott, K. Andrea",
journal = "Physical Review Fluids, Volume 8, Issue 1",
volume = "8",
number = "1",
year = "2023",
publisher = "American Physical Society (APS)",
url = "https://gwf-uwaterloo.github.io/gwf-publications/G23-31001",
doi = "10.1103/physrevfluids.8.014502",
abstract = "Freshwater has been shown to have a maximum density at about four degrees Celsius, and this leads to a phenomenon known as cabbeling. Cabbeling occurs when masses of water on different sides of the temperature of maximum density mix and create a denser mass. What happens when intruding and ambient temperatures in a gravity current are on opposite sides of the temperature of maximum density? How does cabbeling affect the evolution characteristics of gravity currents, and what sort of long term behavior arises?",
}
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<abstract>Freshwater has been shown to have a maximum density at about four degrees Celsius, and this leads to a phenomenon known as cabbeling. Cabbeling occurs when masses of water on different sides of the temperature of maximum density mix and create a denser mass. What happens when intruding and ambient temperatures in a gravity current are on opposite sides of the temperature of maximum density? How does cabbeling affect the evolution characteristics of gravity currents, and what sort of long term behavior arises?</abstract>
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%0 Journal Article %T Gravity currents in the cabbeling regime %A Grace, Andrew %A Stastna, Marek %A Lamb, Kevin G. %A Scott, K. Andrea %J Physical Review Fluids, Volume 8, Issue 1 %D 2023 %V 8 %N 1 %I American Physical Society (APS) %F Grace-2023-Gravity %X Freshwater has been shown to have a maximum density at about four degrees Celsius, and this leads to a phenomenon known as cabbeling. Cabbeling occurs when masses of water on different sides of the temperature of maximum density mix and create a denser mass. What happens when intruding and ambient temperatures in a gravity current are on opposite sides of the temperature of maximum density? How does cabbeling affect the evolution characteristics of gravity currents, and what sort of long term behavior arises? %R 10.1103/physrevfluids.8.014502 %U https://gwf-uwaterloo.github.io/gwf-publications/G23-31001 %U https://doi.org/10.1103/physrevfluids.8.014502
Markdown (Informal)
[Gravity currents in the cabbeling regime](https://gwf-uwaterloo.github.io/gwf-publications/G23-31001) (Grace et al., GWF 2023)
- Gravity currents in the cabbeling regime (Grace et al., GWF 2023)
ACL
- Andrew Grace, Marek Stastna, Kevin G. Lamb, and K. Andrea Scott. 2023. Gravity currents in the cabbeling regime. Physical Review Fluids, Volume 8, Issue 1, 8(1).