| introduction
| multifractals
| clouds | topography
| topography perspective|misc
| movies | covers
| glossary |
publications |
|
|
|
|
| introduction
| multifractals
| clouds | topography
| topography perspective|misc
| movies | covers
| glossary |
publications |
|
| | isotropic cloud | stratified cloud (scale fn) | stratified cloud | cloud fly by|topography fly by|raindrops |space-time | nowcasting | waves | plume | |
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Divergence of realizations, forecasts using conditional expectations (rain nowcasting) The left two show two rain fields which are identical up until t=0, and then diverge afterwards; the far right shows the conditional expectation based on the history up until t=0. Notice that the details disappear quickly since they cannot be forecast very far ahead. The scale is a log scale such as those used in usal radar rain maps. alpha=1.5, C1=0.2, H=0.1. For some of the theory, see Schertzer and Lovejoy 2004 , Marsan et al 1996.
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