Difference between revisions of "Radiation stress"
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Definition|title=Radiation stress | Definition|title=Radiation stress | ||
− | |definition= Radiation stress is the flux of momentum | + | |definition= Radiation stress is the flux of momentum carried by ocean waves. |
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+ | The radiation stress is the momentum transferred through the water body per unit time (the flux of momentum) by wave orbital motion. It is called a stress because for obliquely incident waves, cross-shore momentum can be transferred by both cross-shore wave orbital motion and longshore wave orbital motion and longshore momentum can be transferred by both longshore wave orbital motion and cross-shore wave orbital motion. For obliquely incident waves, a cross-shore gradient in the wave orbital motion, for example due to wave breaking, will exert a stress on the water mass in cross-shore direction as well as in longshore direction. The stress in longshore direction generates a [[longshore current]]. The stress in cross-shore direction generates a [[Wave set-up|water level set-up]] at the coast. | ||
+ | Forcing by radiation stress gradients related to wave breaking is commonly an order of magnitude greater than forcing due to wind stress or other wave nonlinearities</ref>. | ||
For a more detailed explanation, see [[Shallow-water wave theory#Radiation Stress (Momentum Flux)]]. | For a more detailed explanation, see [[Shallow-water wave theory#Radiation Stress (Momentum Flux)]]. | ||
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Revision as of 21:11, 29 June 2022
Definition of Radiation stress:
Radiation stress is the flux of momentum carried by ocean waves.
This is the common definition for Radiation stress, other definitions can be discussed in the article
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The radiation stress is the momentum transferred through the water body per unit time (the flux of momentum) by wave orbital motion. It is called a stress because for obliquely incident waves, cross-shore momentum can be transferred by both cross-shore wave orbital motion and longshore wave orbital motion and longshore momentum can be transferred by both longshore wave orbital motion and cross-shore wave orbital motion. For obliquely incident waves, a cross-shore gradient in the wave orbital motion, for example due to wave breaking, will exert a stress on the water mass in cross-shore direction as well as in longshore direction. The stress in longshore direction generates a longshore current. The stress in cross-shore direction generates a water level set-up at the coast.
Forcing by radiation stress gradients related to wave breaking is commonly an order of magnitude greater than forcing due to wind stress or other wave nonlinearities</ref>.
For a more detailed explanation, see Shallow-water wave theory#Radiation Stress (Momentum Flux).