Changes between Version 2 and Version 3 of gallery/movies/lead

Timestamp:

Jul 8, 2014 9:09:09 AM (10 years ago)

Author:

knoop

Comment:

--

gallery/movies/lead

@@ -1 @@
-== Flow over an ice lead (2006) ==
+= Flow over an ice lead =
 [[TracNav(gallery/toc)]]
-||||='''Flow over an ice lead (2006)''' =||
-{{{#!td style="vertical-align:top; border: 0px solid"
+
+== Flow over an ice lead (2006) #iceflow
+
 {{{#!html
 <embed
@@ -15 +16 @@
 />
 }}}
-}}}
-{{{#!td style="vertical-align:top; border: 0px solid""
+
 '''Project:''' [[imuk/projects/2007_01|The Physics of turbulence over Antarctic leads and polynyas and its parameterization: a joint study using observations, LES and a micro-/mesoscale model]]\\
 \\
 '''Responsible:''' [[imuk/members/witha|Björn Witha]]\\
 \\
-'''Description:''' \\
-Leads in sea ice are responsible for most of the latent and sensible heat transfer from ocean to atmosphere within the marginal ice zones. The animation displays a flow along x (from left to right with a geostrophic wind of about 3 m/s) from sea ice over a lead of 1000m width. The incoming flow is laminar (without turbulence), neutrally stratified, and capped by an inversion above 300m. The surface temperature of ice is assumed to be -23.3C, while the open sea water has a temperature near the freezing point of about -3C. Particles are released near the surface and closely below the inversion. The particle color reflects the buoyancy at the current particle position (red: positive, blue: negative). The particle size is proportional to the magnitude of the vertical velocity component. Cyclic boundary conditions along y are assumed. Convection is generated above the lead but the flow re-stratifies soon after passing the lead. The spatial resolution of the model is still insufficient to resolve the turbulent convection above the first half (upstream part) of the lead.
+'''Description:''' Leads in sea ice are responsible for most of the latent and sensible heat transfer from ocean to atmosphere within the marginal ice zones. The animation displays a flow along x (from left to right with a geostrophic wind of about 3 m/s) from sea ice over a lead of 1000m width. The incoming flow is laminar (without turbulence), neutrally stratified, and capped by an inversion above 300m. The surface temperature of ice is assumed to be -23.3C, while the open sea water has a temperature near the freezing point of about -3C. Particles are released near the surface and closely below the inversion. The particle color reflects the buoyancy at the current particle position (red: positive, blue: negative). The particle size is proportional to the magnitude of the vertical velocity component. Cyclic boundary conditions along y are assumed. Convection is generated above the lead but the flow re-stratifies soon after passing the lead. The spatial resolution of the model is still insufficient to resolve the turbulent convection above the first half (upstream part) of the lead.\\
+
 ||||='''Model Setup'''  =||
 ||Total domain size (x|y|z):||5760m x 1280m x 1477m||
@@ -36 +36 @@
 ||Video Format  ||File size  ||
 ||Flash (.flv)  ||  7.5mb||[[htdocs:gallery/movies/lead.flv|Download]]  ||
-\\
-}}}
+
+----