Titlebook: Air-Ice-Ocean Interaction; Turbulent Ocean Boun Miles McPhee Book 2008 Springer-Verlag New York 2008 Ocean.geophysics.geophysics of sea ice

hypnogram

affect mixing in the Weddell Sea...The book’s content, developed from a series of lectures, may be appropriate additional material for upper-level undergraduates and first-year graduate students studying the g978-1-4419-2685-2978-0-387-78335-2

CUR

大罵

Grating

Receive

Gobble

A Numerical Model for the Ice/Ocean Boundary Layer,rd and Baumert 1995) models in that the length scales are based on a combination of measurements and similarity theory, rather than derived from separate TKE and master length scale conservation equations. A practical impact is that the LTC model eliminates the need to carry these equations in the s

AGATE

LTC Modeling Examples,rgetic inertial motion of the ice and upper ocean. Inertial oscillation nearly always implies strong shear in the upper part of the pycnocline, and early models of mixed-layer evolution (e.g., Pollard et al. 1973; Niiler and Kraus 1977) related the rate of mixed-layer deepening (“entrainment velocit

易改變

lambaste

https://doi.org/10.1007/978-3-662-67084-2mosphereocean exchanges and how studies of turbulent exchange in the ice-ocean boundary layer have revealed much about how planetary boundary layers (where rotation is important) work in general. It briefly describes pertinent ice-station exercises, and lays out the framework for subsequent chapters

Gentry

Patrick Glogner-Pilz,Patrick S. F?hlilarity theory for the IOBL stabilized by positive buoyancy flux at the surface (melting). The crucial parameters identified in the exercise, including important turbulence scales, then provide the rationale for development of the local turbulence closure model described in subsequent chapters.