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  1. Semi-arid climate - Wikipedia

    en.wikipedia.org › wiki › Hot_semi-arid_climate

    Hot semi-arid climates (type "BSh") tend to be located in the 20s and 30s latitudes of the (tropics and subtropics), typically in proximity to regions with a tropical savanna or a humid subtropical climate. These climates tend to have hot, sometimes extremely hot summers and warm to cool winters, with some to minimal precipitation.

  2. Köppen climate classification - Wikipedia

    en.wikipedia.org › wiki › Köppen_climate_classification

    BWk = Cold desert climate; BSh = Hot semi-arid climate; BSk = Cold semi-arid climate; Group C: Temperate climates. This type of climate has the coldest month averaging between 0 °C (32 °F) (or −3 °C (27 °F)) and 18 °C (64.4 °F) and at least one month averaging above 10 °C (50 °F).

  3. Semi-arid climate — Wikipedia Republished // WIKI 2

    wiki2.org › en › Semi-arid_climate
    • Defining Attributes of semi-arid Climates
    • Hot semi-arid Climates
    • Cold semi-arid Climates
    • Regions of Varying Classification
    • See Also

    A more pre­cise de­f­i­n­i­tion is given by the Köppen cli­mate clas­si­fi­ca­tion, which treats steppe cli­mates (BSk and BSh) as in­ter­me­di­ates be­tween desert cli­mates (BW) and humid cli­mates in eco­log­i­cal char­ac­ter­is­tics and agri­cul­tural po­ten­tial. Semi-arid cli­mates tend to sup­port short or scrubby veg­e­ta­tion and are usu­ally dom­i­nated by ei­ther grasses or shrubs. To de­ter­mine if a lo­ca­tion has a semi-arid cli­mate, the pre­cip­i­ta­tion thresh­old must first be de­ter­mined. The method used to find the pre­cip­i­ta­tion thresh­old (in mil­lime­ters): 1. multiplying by 20 the average annual temperature in degrees Celsius and then 1.1. adding 280 if at least 70% of the total precipitation falls in the high-sun half of the year (April–September in the northern hemisphere, October–March in the southern hemisphere) 1.2. adding 140 if 30–70% of the total precipitation falls in the high-sun half of the year 1.3. not adding anything if less than 30% of the...

    Hot semi-arid cli­mates (type "BSh") tend to be lo­cated in the 20s and 30s lat­i­tudes of the (trop­ics and sub­trop­ics), typ­i­cally in prox­im­ity to re­gions with a trop­i­cal sa­vanna or a humid sub­trop­i­cal cli­mate. These cli­mates tend to have hot, some­times ex­tremely hot sum­mers and warm to cool win­ters, with some to min­i­mal pre­cip­i­ta­tion. Hot semi-arid cli­mates are most com­monly found around the fringes of sub­trop­i­cal deserts. Hot semi-arid cli­mates are most com­monly found in Africa, Aus­tralia and South Asia. In Aus­tralia, a large por­tion of the Out­back sur­round­ing the cen­tral desert re­gions lies within the hot semi-arid cli­mate region.[clarification needed] In South Asia, both India and sec­tions of Pak­istan ex­pe­ri­ences the sea­sonal ef­fects of mon­soons and fea­ture short but well-de­fined wet sea­sons, but is not suf­fi­ciently wet over­all to qual­ify as a trop­i­cal sa­vanna cli­mate. Hot semi-arid cli­mates can also be found in Eu­ro...

    Cold semi-arid cli­mates (type "BSk") tend to be lo­cated in el­e­vated por­tions of tem­per­ate zones, typ­i­cally bor­der­ing a humid con­ti­nen­tal cli­mate or a Mediter­ranean cli­mate. They are typ­i­cally found in con­ti­nen­tal in­te­ri­ors some dis­tance from large bod­ies of water. Cold semi-arid cli­mates usu­ally fea­ture warm to hot dry sum­mers, though their sum­mers are typ­i­cally not quite as hot as those of hot semi-arid cli­mates. Un­like hot semi-arid cli­mates, areas with cold semi-arid cli­mates tend to have cold win­ters. These areas usu­ally see some snow­fall dur­ing the win­ter, though snow­fall is much lower than at lo­ca­tions at sim­i­lar lat­i­tudes with more humid cli­mates. Areas fea­tur­ing cold semi-arid cli­mates tend to have higher el­e­va­tions than areas with hot semi-arid cli­mates, and tend to fea­ture major tem­per­a­ture swings be­tween day and night, some­times by as much as 20°C (36°F) or more in that time frame. These large di­ur­nal tem­p...

    In cli­mate clas­si­fi­ca­tion, three isotherms means that de­lin­eate be­tween hot and cold semi-arid cli­mates — the 18 °C (64 °F) av­er­age an­nual tem­per­a­ture or that of the cold­est month (0 or −3 °C (32 or 27 °F)), the warm side of the isotherm of choice defin­ing a BSh cli­mate from the BSk on the cooler side. As a re­sult of this, some areas can have cli­mates that are clas­si­fied as hot or cold semi-arid de­pend­ing on the isotherm used. One such lo­ca­tion is San Diego, Cal­i­for­nia (at its main air­port), which has cool sum­mers for the lat­i­tude due to pre­vail­ing winds off the ocean (so the av­er­age an­nual tem­per­a­ture is below 18 °C (64 °F)) but mild win­ters (av­er­age tem­per­a­ture in Jan­u­ary, 14 °C (57 °F), and closer to the 18.0 °C (64.4 °F) isotherm that sep­a­rates trop­i­cal and sub­trop­i­cal cli­mates than to the 0 or −3 °C (32 or 27 °F) isotherm for the cold­est month that sep­a­rates tem­per­ate and con­ti­nen­tal cli­mates).

  4. Climate - Wikipedia

    en.wikipedia.org › wiki › Climate

    A tropical savanna is a grassland biome located in semi-arid to semi-humid climate regions of subtropical and tropical latitudes, with average temperatures remaining at or above 18 °C (64 °F) all year round, and rainfall between 750 millimetres (30 in) and 1,270 millimetres (50 in) a year.

    • Defining Attributes of semi-arid Climates
    • Hot semi-arid Climates
    • Cold semi-arid Climates
    • Regions of Varying Classification
    • See Also

    A more precise definition is given by the Köppen climate classification, which treats steppe climates (BSk and BSh) as intermediates between desert climates (BW) and humid climates in ecological characteristics and agricultural potential. Semi-arid climates tend to support short or scrubby vegetation and are usually dominated by either grasses or shrubs. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. The method used to find the precipitation threshold (in millimeters): 1. multiplying by 20 the average annual temperature in degrees Celsius and then 1.1. adding 280 if at least 70% of the total precipitation falls in the high-sun half of the year (April–September in the northern hemisphere, October–March in the southern hemisphere) 1.2. adding 140 if 30–70% of the total precipitation falls in the high-sun half of the year 1.3. not adding anything if less than 30% of the total precipitation falls in the high-sun half of the year...

    Hot semi-arid climates (type "BSh") tend to be located in the 20s and 30s latitudes of the (tropics and subtropics), typically in proximity to regions with a tropical savanna or a humid subtropical climate. These climates tend to have hot, sometimes extremely hot, summers and warm to cool winters, with some to minimal precipitation. Hot semi-arid climates are most commonly found around the fringes of subtropical deserts. Hot semi-arid climates are most commonly found in Africa, Australia and South Asia. In Australia, a large portion of the Outback surrounding the central desert regions lies within the hot semi-arid climate region.[clarification needed] In South Asia, both India and sections of Pakistan experiences the seasonal effects of monsoons and feature short but well-defined wet seasons, but is not sufficiently wet overall to qualify as a tropical savanna climate. Hot semi-arid climates can also be found in Europe, primarily in Southeast Spain and parts of Greece, Italy, Portu...

    Cold semi-arid climates (type "BSk") tend to be located in elevated portions of temperate zones, typically bordering a humid continental climate or a Mediterranean climate. They are typically found in continental interiors some distance from large bodies of water. Cold semi-arid climates usually feature warm to hot dry summers, though their summers are typically not quite as hot as those of hot semi-arid climates. Unlike hot semi-arid climates, areas with cold semi-arid climates tend to have cold winters. These areas usually see some snowfall during the winter, though snowfall is much lower than at locations at similar latitudes with more humid climates. Areas featuring cold semi-arid climates tend to have higher elevations than areas with hot semi-arid climates, and tend to feature major temperature swings between day and night, sometimes by as much as 20°C (36°F) or more in that time frame. These large diurnal temperature variations are seldom seen in hot semi-arid climates. Cold...

    In climate classification, three isotherms means that delineate between hot and cold semi-arid climates — the 18 °C (64 °F) average annual temperature or that of the coldest month (0 or −3 °C (32 or 27 °F)), the warm side of the isotherm of choice defining a BSh climate from the BSk on the cooler side. As a result of this, some areas can have climates that are classified as hot or cold semi-arid depending on the isotherm used. One such location is San Diego, California (at its main airport), which has cool summers for the latitude due to prevailing winds off the ocean (so the average annual temperature is below 18 °C (64 °F)) but mild winters (average temperature in January, 14 °C (57 °F), and closer to the 18.0 °C (64.4 °F) isotherm that separates tropical and subtropical climates than to the 0 or −3 °C (32 or 27 °F) isotherm for the coldest month that separates temperate and continental climates).

  5. Semi-arid climate - Wikipedia | WordDisk

    worddisk.com › wiki › Hot_semi-arid_climate

    A semi-arid climate, semi-desert climate, or steppe climate is the climate of a region that receives precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes.

  6. What Are The Characteristics Of A Semi-arid Climate Pattern ...

    www.worldatlas.com › articles › what-are-the

    Nov 13, 2017 · Hot semi-arid climates characterize the tropics and sub-tropics located in the 20s and 30s latitudes. They are often located near the tropical savanna climate or on the fringe of sub-tropical desert climate. Hot semi-desert climate is known for hot summer and cool winter, with relatively low precipitation.

  7. Semi-arid climate - Wiki - Wikiredia

    en.wikiredia.com › wiki › Semi-arid_climate

    Hot semi-arid climates (type "BSh") tend to be located in the 20s and 30s latitudes of the (tropics and subtropics), typically in proximity to regions with a tropical savanna or a humid subtropical climate. These climates tend to have hot, sometimes extremely hot, summers and warm to cool winters, with some to minimal precipitation.

  8. Semi-arid climate - YouTube

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    A semi-arid climate or steppe climate are climatic regions that receive precipitation below potential evapotranspiration, but not extremely. A more precise d...

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  9. Semi-arid climate - Infogalactic: the planetary knowledge core

    infogalactic.com › info › Semi-arid_climate
    • Hot semi-arid Climates
    • Cold semi-arid Climates
    • Regions of Varying Classification
    • See Also

    Hot semi-arid climates (type "BSh") tend to be located in the tropics and subtropics. These climates tend to have hot, sometimes extremely hot, summers and mild to warm winters. Snow rarely (if ever) falls in these regions. Hot semi-arid climates are most commonly found around the fringes of subtropical deserts. The most common variant of a hot semi-arid climate, found in regions such as West Africa, India, parts of Mexico and bordering areas in Texas, parts of Southern California, and small parts of Pakistan experiences the seasonal effects of monsoons and has a short but well-defined wet season, but is not sufficiently wet overall to qualify as a tropical savanna climate. In Australia, a large portion of the Outback surrounding the central desert regions, lies within the hot semi-arid climate regime.[clarification needed] Hot semi-arid climates can also be found in sections of South America such as the sertão and on the poleward side of the arid deserts where they typically featur...

    Cold semi-arid climates (type "BSk") tend to be located in temperate zones. They are typically found in continental interiors some distance from large bodies of water. Cold semi-arid climates usually feature hot and dry (often exceptionally hot) summers, though their summers are typically not quite as hot as those of hot semi-arid climates. Unlike hot semi-arid climates, areas with cold semi-arid climates tend to have cold winters. These areas usually see some snowfall during the winter, though snowfall is much lower than at locations at similar latitudes with more humid climates. Areas featuring cold semi-arid climates tend to have higher elevations than areas with hot semi-arid climates, and are sometimes subject to major temperature swings between day and night, sometimes by as much as 20 °C (36 °F) or more in that time frame. These large diurnal temperature variations are seldom seen in hot semi-arid climates. Cold semi-arid climates at higher latitudes tend to have dry winters...

    Three isotherms means that delineate between hot and cold semi-arid climates — the 18°C average annual temperature or that of the coldest month (0°C or −3°C), the warm side of the isotherm of choice defining a BSh climate from the BSk on the cooler side. As a result of this, some areas can have climates that are classified as hot or cold semi-arid depending on the isotherm used. One such location is San Diego, California(at its main airport), which has cool summers for the latitude due to prevailing winds off the ocean (so the average annual temperature is below 18°C) but mild winters (average temperature in January, 14°C, and closer to the 18.0°C isotherm that separates tropical and subtropical climates than to the 0°C or −3°C isotherm for the coldest month that separates temperate and continental climates).

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