nasal conchae
The prominent bony ridges on the lateral walls of the nasal cavity are called the turbinates or nasal conchae. They help increase the surface area of the nasal cavity to facilitate warming, humidifying, and filtering of the air before it reaches the lungs.
The bony projections are called the superior, middle and inferior conchae. They increase surface area to warm and moisten incoming air.
It's called a warm front.
Rising warm air is called convection. As warm air rises, it creates convection currents that circulate heat and moisture in the atmosphere.
When a warm air mass moves into an area where a cold air mass is located, it is called a warm front. At a warm front, the warm air mass rises over the cold air mass, leading to gradual temperature increases and cloud formation.
This is a warm front.
When warm air is lifted up over cold air, it is called "overrunning" or "warm air advection." This process leads to the warm air rising, cooling, and condensing to form clouds and precipitation as it interacts with the cold air at the surface.
Regions of cold heavy air are called highs. As cool air moves under warm air, the warm air is pushed upward.
The upward movement of warm air is called convection. This process occurs as warm air rises due to its lower density compared to cooler air, creating vertical air currents in the atmosphere.
Actually, when the warm air mass overtakes the cold air, it is called a warm front. A warm front typically brings gradual changes in weather, such as increasing temperatures, and is often associated with gentle rain or snow.
Warm front
warm front