WARM AIR CIRCULATION PROMOTING DEVICE IN WALLPROBLEM TO BE SOLVED: To circulate warm air between a sealed space below a floor and a space in a wall by utilizing natural convection.FUKUSHIMA TAKAKO福嶋 多可子ARAKI AKIO荒木 章夫SAKAMOTO YOSHIHITO...
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...
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...
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...
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 ...
Then the samples were dried to constant mass (± 2%) in an air convection oven at 60 ± 1 °C for at least 1 h. Thereafter, the samples were ground, sieved through a < 0.25 mm fil- ter. 200 mg of milled sample was heated at 150 ± 1 °C for ten minutes, and...
Although CAPE provides insight into whether the atmosphere has the potential to produce deep moist convection, convective initiation is necessary for the thunderstorm to occur. This problem is highlighted over locations such as southern Texas or the western Mediterranean Sea where high CAPE rarely result...
一次切断低压诱发的暖区深对流与异常副热带锋及其平流层-对流层交换 Stratosphere-troposphere exchange corresponding to a deep convection in warm sector and abnormal subtropical front induced by a cutoff low over East Asia 2014. Strat~ osphere-troposphere exchange corresponding to a deep convection in the...
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...
This research conducts a study of natural convection heat transfer (NCHT) in a nanofluid under a magnetic field (MF). The nanofluid is in a cavity inclined at an angle of 45°. The MF can take different angles between 0° and 90°. Radiative heat transfer is present in the cavity in ...