Inversions, and fog, stratus and cumulus formation in warm air over cooler water - Telford, Chai - 1984 () Citation Context ...as the most useful indicator of sea fog formation, while coastal fogs were mainly associated with a low level inversion that may be caused by radiative cooling at...
On the contrary, the heavy rain at night highlighted the importance of locally enhanced baroclinicity due to intrusion of cold air. Elevated convection was triggered by the lifting of the SW warmer air above the shallow cold surface to form stagnant convection in the basin. Convective cells that...
Here we propose that the AMOC demise is caused by a Summer-Fall pulse of warm air/water temperature, followed by a Winter sea ice melting over the Arctic and a Spring southward advection of fresher/cooler waters by ocean currents. The recovery of the AMOC, on the other hand, is attributed...
The F96 warm-layer model modified for 24 hour integration Because a linear temperature profile above the trapping depth is assumed, the warm-layer temperature change at the air–sea interface will be double the layer-averaged temperature change, that is, ΔTwarm = 2ΔTlayer. As shown...
Air Fry Yes Self Clean Yes Steam Clean No Wi-Fi Connection Yes Easy Cook No Healthy Cook No Favorite Cook Yes Keep Warm Yes Clock Yes Numeric Pad No Kitchen Timer Yes Child Safety Lock Yes Hidden Bake Element No Interior Light (Position) 1 Incandescent 40W(Back) Light (Lamp) On/Off Yes...
The bright kitchen is updated with white cabinetry, granite countertops, stainless steel appliances, plus a newer convection oven with electric induction cooktop and refrigerator. On one side, the kitchen opens to a cozy sunporch-your go-to morning coffee spot. On the other, it leads to a ...
As long as the air closest to the surface remains slightly warmer than the air above it, this convective vertical mixing process will continue. However, when the convection process is reversed or inhibited and the air closest to the surface becomes cooler than the air above it, a temperature ...
, climate model simulations, and idealized box model experiments point to the subpolar gyre as a key coupling region where vigorous wind systems encounter the southernmost extension of sea ice and the most variable currents of the North Atlantic, with connections to the deep ocean via convection....
Deep convection over the western tropical Pacific warm pool is analyzed in terms of its relation to the atmospheric Kelvin-Rossby wave, which dominates the large-scale flow during the austral summer. The study uses Doppler radar data collected by aircraft and ship radars during different time perio...
12. Air-sea heat and freshwater fluxes regulate the transformation of surface water masses and deep ocean mixing13. Prominent regions of ocean interior oxygenation include the subpolar North Atlantic, where strong surface buoyancy loss triggers open-ocean convection14, the coastal regions around ...