30 kilometers wide
30 kilometer wide
Piedmont and mesa
The area where warm and cold seawater combine is known as a thermocline. This is a layer in the ocean where there is a rapid change in temperature. The mixing of warm and cold water at the thermocline is crucial for various oceanic processes and marine life.
Piedmont and Mesa
Zaire is located near the equator in Africa, so it falls primarily within the torrid zone. This means it experiences high temperatures and humidity throughout the year.
The temperature in the zone beneath the thermocline remains relatively stable as it experiences minimal mixing with the warmer water above and the cooler water below. This results in a sharp temperature gradient between the layers above and below the thermocline.
Most air has humidity. When there is humidity, then there is a dew point - a temperature - below which the humidity condenses into water droplets. If you are in an air-conditioned space (at equilibrium), your glasses are cool. You walk into a warmer zone - one which has a dew point above the temperature of your glasses - and you get condensation.
The boundary between cold and warm air masses is called a front. Fronts typically form where two air masses with different temperatures, humidity levels, and densities meet. This transition zone can result in weather changes such as clouds, precipitation, and temperature shifts.
suface zone and thermocline zone
The UK is in the temperate maritime climate zone, characterized by mild temperatures, high humidity, and relatively small temperature variations throughout the year. This is due to the influence of the Atlantic Ocean which helps moderate the climate.
Mixing zone
temperate zone