Hasselman, 1976 in the asymptotic limit where complicating processes such as advective and diffusive exchanges of heat with the deep ocean are ignored e.g.    From Wordnik.com.  [Climate Insensitivity and AR(1) Models « Climate Audit] Reference

These include turbluent mixing, advective and convective processes, as well as mecanical mixing.    From Wordnik.com.  [Letter to NAS « Climate Audit] Reference

This is very likely to alter the advective pathways and basin residence times of sea ice formed in winter on the Eurasian shelves.    From Wordnik.com.  [Anticipated changes in physical conditions in the Arctic] Reference

On the exposed hills and ridges facing southwest, the phenomenon of advective fog occurs, bringing moisture to the desert and leading to lomas vegetation.    From Wordnik.com.  [Sechura desert] Reference

Given the near dearth of empirical observations, measurements, and actual knowledge about the effects of carbon aerosols and cloud formations upon convective, advective, and radiative heat transport mechanisms in the atmosphere, how can any claims or conclusions about the effects of emissions be reasonably supportable as a true application of science?.    From Wordnik.com.  [RMS and Sulphate Emissions « Climate Audit] Reference

Our measurements provide evidence for a rapid advective pathway for the transmission of oceanic variability to the ice-sheet margins.    From Wordnik.com.  [Naturejobs - All Jobs] Reference

These include components of suggested periodic nature, large-scale advective effects, regional processes, and atmospheric teleconnections.    From Wordnik.com.  [Scientific Blogging] Reference

These modifications take the vertical gradient of the Exner function perturbation into account, with an on-off coefficient to account for the role of the advective terms.    From Wordnik.com.  [Climate Science: Roger Pielke Sr. Research Group News] Reference

Mass average flux resulting from combined advection and diffusion is shown to be evaluated as the vector sum of advective and diffusive fluxes, rather than diffusive flux being evaluated as a flux relative to a mass average flux.    From Wordnik.com.  [PhysOrg.com - latest science and technology news stories] Reference

Additiona lly, the biggest limiting factor to instability normally is lack of sunshine - and while that will be at play with increasing moisture in the mid-levels ahead of the front, the advective properties of the strong southwest wind should be able to force the warm front far north, to near the Canadian border, thereby allowing warm air to penetrate across most of New England.    From Wordnik.com.  [MATTNOYES.NET - Weather Website & Blog] Reference

The formalistic inclusion of the advective terms in the new equation gives almost no additional improvement of the simulated precipitation. ".    From Wordnik.com.  [Climate Science: Roger Pielke Sr. Research Group News] Reference