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The Köppen climate classification system was modified further within the Trewartha climate classification system in 1966 (revised in 1980). The Trewartha system sought to create a more refined middle latitude climate zone, which was one of the criticisms of the Köppen system (the climate group C was too general). [10]: 200–1
Regions where oceanic or subtropical highland climates (Cfb, Cfc, Cwb, Cwc) are found. An oceanic climate, also known as a marine climate or maritime climate, is the temperate climate sub-type in Köppen classification represented as Cfb, typical of west coasts in higher middle latitudes of continents, generally featuring cool to warm summers and cool to mild winters (for their latitude), with ...
Today, the most commonly used climate map is the Köppen climate classification, developed by Russian climatologist of German descent and amateur botanist Wladimir Köppen (1846–1940), which divides the world into five major climate regions, based on average annual precipitation, average monthly precipitation, and average monthly temperature.
The Mid Atlantic Bight's ecosystem can be seen as a transitional ecosystem between that of temperate and tropical ocean. Like the Gulf of Maine, it is an area of relatively high primary production. Much of the primary production in the Mid Atlantic Bight is in the summer and winter, and is highest near shore, and in estuarine environments.
The Atlantic meridional overturning circulation (AMOC) is the main ocean current system in the Atlantic Ocean. [ 1 ] : 2238 It is a component of Earth's ocean circulation system and plays an important role in the climate system .
The Bahamas map of Köppen climate classification. The climate of the Bahama islands is mostly tropical savanna , with two seasons, a hot and wet summer (wet season) and dry winter (dry season). During the wet season, which extends from May through October, the climate is dominated by warm, moist tropical air masses [ 1 ] as the Bermuda High ...
In the Atlantic, the area between 10°N and 20°N spawns the most hurricanes in a given season because of the warmer temperatures. Hurricanes do not form outside this range because nearer to the equator the Coriolis effect is not strong enough to create the tight circulation needed, and farther north the temperatures are too cool. [5]
Holdridge life zone classification scheme. Although conceived as three-dimensional by its originator, it is usually shown as a two-dimensional array of hexagons in a triangular frame. Map of the world using hexagons of the same area, with landmasses and oceans categorized as different Lifezones, also arranged hexagonally