This list of locations with a subtropical climate specifically lists locations considered within the
subtropics. The subtropics are geographic and
climate zones located roughly between the
Tropic of Cancer and
Tropic of Capricorn and the 40th parallel in both hemispheres. Subtropical climate regions can exist at high elevations within the
tropics, such as across the
Mexican Plateau and the
Ethiopian Highlands and in
Da Lat of the
Vietnamese Central Highlands. These regions can also exist beyond 45 degrees poleward due to maritime influences on the NW European and Argentinian coasts, according to Trewartha.
Six climate classifications utilise the term to help define the various
temperature and
precipitation regions for the planet
Earth. Using the
Trewartha climate classification eight or more months of the year within the subtropics have an average temperature at or above 10 °C (50 °F). The
Köppen climate classification instead classifies the warmest month above 22 °C (71.6 °F) and the coldest above 0 °C (32 °F) or −3 °C (26.6 °F) depending on preference. Under both classifications, at least one month must average below 18 °C (64.4 °F) or the climate is considered tropical.
Leslie Holdridge defined the subtropical climates as having a mean annual
biotemperature between the frost line or critical temperature line, 16 °C to 18 °C (depending on locations in the world) and 24 °C.[1] The frost line separates the warm temperate region from the subtropical region. It represents the dividing line between two major physiological groups of evolved plants. On the warmer side of the line, the majority of the plants are sensitive to low temperatures. They can be killed back by frosts as they have not evolved to withstand periods of cold. On the colder temperate side of the line, the total flora is adapted to survive periods of variable length of low temperatures, whether as seeds in the case of the annuals or as perennial plants which can withstand the cold. The [16 °C-18 °C] segment is often "simplified" as 17 °C (= 2(log212+0;5) ≈ 16.97 °C).[2]
The Holdridge subtropical climates straddle more or less the warmest subtropical climates and the less warm tropical climates as defined by the Köppen-Geiger or Trewartha climate classifications.
However
Wladimir Köppen has distinguished the hot or subtropical and tropical (semi-)arid climates (BWh or BSh) having an average annual temperature greater than or equal to 18 °C (64.4 °F) from the cold or temperate (semi-)arid climates (BWk or BSk) whose annual temperature average is lower.[3] This definition, though restricted to dry regions, is almost similar to Holdridge's.
A great portion of the world's deserts are located within the subtropics, due to the development of the
subtropical ridge. Within the
humid monsoon regions in the subtropics such as Northern Vietnam (including
Hanoi), a
wet season is seen annually during the summer, which is when most of the yearly rainfall falls. Within the
Mediterranean climate region, the wet season occurs during the winter. Areas bordering warm oceans are prone to locally heavy rainfall from
tropical cyclones, which can contribute a significant percentage of the annual rainfall. Plants such as
date palms,
citrus,
mango,
litchi, and
avocado are grown within the subtropical zones.
This is not a complete list and is not intended to be one. Many of the higher mountains at tropical latitudes have sparsely (if at all) inhabited areas with a subtropical climate.
Africa
^1 Only in Trewartha's classification. ^2 Which borders on a fully tropical climate.
^Mackintosh, Lesley (28 February 2007).
"Overview of New Zealand Climate | NIWA". NIWA. The National Institute of Water and Atmospheric Research. Retrieved 15 August 2013.
This list of locations with a subtropical climate specifically lists locations considered within the
subtropics. The subtropics are geographic and
climate zones located roughly between the
Tropic of Cancer and
Tropic of Capricorn and the 40th parallel in both hemispheres. Subtropical climate regions can exist at high elevations within the
tropics, such as across the
Mexican Plateau and the
Ethiopian Highlands and in
Da Lat of the
Vietnamese Central Highlands. These regions can also exist beyond 45 degrees poleward due to maritime influences on the NW European and Argentinian coasts, according to Trewartha.
Six climate classifications utilise the term to help define the various
temperature and
precipitation regions for the planet
Earth. Using the
Trewartha climate classification eight or more months of the year within the subtropics have an average temperature at or above 10 °C (50 °F). The
Köppen climate classification instead classifies the warmest month above 22 °C (71.6 °F) and the coldest above 0 °C (32 °F) or −3 °C (26.6 °F) depending on preference. Under both classifications, at least one month must average below 18 °C (64.4 °F) or the climate is considered tropical.
Leslie Holdridge defined the subtropical climates as having a mean annual
biotemperature between the frost line or critical temperature line, 16 °C to 18 °C (depending on locations in the world) and 24 °C.[1] The frost line separates the warm temperate region from the subtropical region. It represents the dividing line between two major physiological groups of evolved plants. On the warmer side of the line, the majority of the plants are sensitive to low temperatures. They can be killed back by frosts as they have not evolved to withstand periods of cold. On the colder temperate side of the line, the total flora is adapted to survive periods of variable length of low temperatures, whether as seeds in the case of the annuals or as perennial plants which can withstand the cold. The [16 °C-18 °C] segment is often "simplified" as 17 °C (= 2(log212+0;5) ≈ 16.97 °C).[2]
The Holdridge subtropical climates straddle more or less the warmest subtropical climates and the less warm tropical climates as defined by the Köppen-Geiger or Trewartha climate classifications.
However
Wladimir Köppen has distinguished the hot or subtropical and tropical (semi-)arid climates (BWh or BSh) having an average annual temperature greater than or equal to 18 °C (64.4 °F) from the cold or temperate (semi-)arid climates (BWk or BSk) whose annual temperature average is lower.[3] This definition, though restricted to dry regions, is almost similar to Holdridge's.
A great portion of the world's deserts are located within the subtropics, due to the development of the
subtropical ridge. Within the
humid monsoon regions in the subtropics such as Northern Vietnam (including
Hanoi), a
wet season is seen annually during the summer, which is when most of the yearly rainfall falls. Within the
Mediterranean climate region, the wet season occurs during the winter. Areas bordering warm oceans are prone to locally heavy rainfall from
tropical cyclones, which can contribute a significant percentage of the annual rainfall. Plants such as
date palms,
citrus,
mango,
litchi, and
avocado are grown within the subtropical zones.
This is not a complete list and is not intended to be one. Many of the higher mountains at tropical latitudes have sparsely (if at all) inhabited areas with a subtropical climate.
Africa
^1 Only in Trewartha's classification. ^2 Which borders on a fully tropical climate.
^Mackintosh, Lesley (28 February 2007).
"Overview of New Zealand Climate | NIWA". NIWA. The National Institute of Water and Atmospheric Research. Retrieved 15 August 2013.