The "low latitudes" are those near the equator, in the tropics, etc.
Countries found in that region include those in Central America, the west Indies,
northern South America, central and Saharan Africa, southern India, Sri Lanka,
Thailand, Laos, Vietnam, Indonesia, the Philippines, and the islands of the south
Pacific.
The two main types of dry climates are semi-arid (or steppe) and arid (or desert), both of which occur in low latitudes and midlatitudes.
Countries in the midlatitudes benefit from rainfall in Mediterranean highland and humid subtropical climates by supporting agriculture, enhancing water supply, and maintaining biodiversity. The Mediterranean climate, characterized by wet winters and dry summers, allows for the cultivation of diverse crops, including olives and grapes. Similarly, humid subtropical regions receive ample rainfall, fostering lush vegetation and productive farmland. These climatic conditions contribute to economic stability and food security in these regions.
The most variable weather on Earth is typically found in regions known as "weather transition zones," such as the mid-latitudes where cold polar air masses meet warm tropical air masses, leading to diverse and often unpredictable weather patterns. Areas prone to frequent cyclones, such as the Tropics and mid-latitude regions, also experience highly variable weather conditions.
The closer your location is to the equator, the hotter it will be. This is where you can expect hurricanes, tropical storms, spotty rain clouds, and lots of sun. The farther you are located from the equator, the colder it will be. You would expect more rain and snow, and less sun.
The majority of wind and ocean currents are formed by the uneven heating and cooling of the medium in question. The convection currents which result from this heating and cooling drive the atmospheric patterns of the atmosphere. Specific currents are shaped by the terrain, and many other factors, including the earths rotation.
Near the equator.
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The two main types of dry climates are semi-arid (or steppe) and arid (or desert), both of which occur in low latitudes and midlatitudes.
Howard B. Bluestein has written: 'Clouds' 'Tornado alley' -- subject- s -: Tornadoes, Storms, Pictorial works 'Synoptic-Dynamic Meteorology in Midlatitudes: Volume II'
The ocean current flowing along the west coast of a continent in the midlatitudes tends to be cooler compared to ocean currents along the east coast due to upwelling of colder water from deeper layers. This phenomenon brings nutrient-rich water to the surface, supporting diverse marine ecosystems. Examples include the California Current off the west coast of North America, which contributes to the cooler temperatures in that region.
No. Some regions have much higher tornado frequencies than other. For example, the central plains of the United States (a region called tornado alley) experiences more tornadoes than anywhere else in the world, but west of the Rockies tornadoes are relatively rare.
The geostrophic wind component is the result of the balance between Coriolis force and pressure gradient force. It flows parallel to isobars and approximates the flow above the atmospheric boundary layer in the midlatitudes.
It's called membrane potential.
Polar easterlies are dry, cold prevailing winds that blow from the east. They emanate from the polar highs, areas of high pressure around the North and South Poles. Polar easterlies flow to low-pressure areas in sub-polar regions. Westerlies are prevailing winds that blow from the west at midlatitudes.
From Wikipedia, the free encyclopediaThe mid-latitudes (sometimes midlatitudes) are the areas on earth between the tropics and the polar regions, approximately 30° to 60° north or south of the equator. The mid-latitudes are an important region in meteorology, having weather patterns which are generally distinct from weather in the tropics and the polar regions. Weather fronts and extratropical cyclones are usually found in this area, as well as occasional tropical cyclones which have traveled from their areas of formation closer to the equator.
Ocean water is usually saltiest near the surface. High levels of evaporation at the surface cause a reduction in freshwater and thus create saltier water near the surface. This effect is most dominant in the warm tropical areas around the equator, thus these areas are saltier than in midlatitudes. Since high salinity implies denser, and thus heavier, water, one might suspect that the saltiest water sinks to the bottom. However, temperature effects tend to dominate the vertical stratification.