Convective updrafts near sea-breeze fronts

Measuring the sea breeze from QuikSCAT Scatterometry

[1] Differences between morning and evening winds from QuikSCAT scatterometer measurements are analyzed to diagnose the diurnal variability of the wind over the ocean. A statistically significant signal, associated with the sea breeze, is present along most of the world’s coastlines. Significant diurnal variability is also present mid-ocean in the easterly trade wind belts.

Sea Breeze: Structure, Forecasting, and Impacts

[1] The sea breeze system (SBS) occurs at coastal locations throughout the world and consists of many spatially and temporally nested phenomena. Cool marine air propagates inland when a cross-shore mesoscale (2–2000 km) pressure gradient is created by daytime differential heating. The circulation is also characterized by rising currents at the sea breeze front and diffuse sinking currents well ...

Transitions between convective patterns in chemical fronts.

Linear stability analysis of convective chemical fronts

Sea urchin feeding fronts

Sea urchin feeding fronts are a striking example of spatial pattern formation in an ecological system. If it is assumed that urchins are asocial, and that they move randomly, then the formation of these dense fronts is an apparent paradox. The key lies in observations that urchins move further in areas where their algal food is less plentiful. This naturally leads to the accumulation of urchins...