[[File:BS climate.png|thumb|upright=1.75|Regions with semi-arid climates
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A semi-arid climate, semi-desert climate, or steppe climate is a aridity sub-type. It is located on regions that receive 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 .
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):
If the area's annual precipitation in millimeters is less than the threshold but more than half or 50% the threshold, it is classified as a BS (steppe, semi-desert, or semi-arid climate).
Furthermore, to delineate hot semi-arid climates from cold semi-arid climates, a mean annual temperature of is used as an isotherm. A location with a BS-type climate is classified as hot semi-arid ( BSh) if its mean temperature is above this isotherm, and cold semi-arid ( BSk) if not.
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. In South Asia, both India and parts of Pakistan experience the seasonal effects of and feature short but well-defined , but are not sufficiently wet overall to qualify as either a tropical savanna or a humid subtropical climate.
Hot semi-arid climates can be also found in parts of North America, such as most of northern Mexico, the ABC Islands, the of Hispaniola's mountain ranges in the Dominican Republic and Haiti, parts of the Southwestern United States including California's Central Valley, and sections of South America such as the sertão, the Gran Chaco, and the poleward side of the arid deserts, where they typically feature a Mediterranean precipitation pattern, with generally rainless summers and wetter winters. They are also found in few areas of Europe surrounding the Mediterranean Basin. In Europe, BSh climates are predominantly found in southeastern Spain. It can also be found primarily in parts of south Greece but also in marginal areas of Thessaloniki and Chalkidiki in north Greece, most of Formentera, marginal areas of Ibiza and marginal areas of Italy in Sicily, Sardinia and Lampedusa.
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. 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 and wetter summers, while cold semi-arid climates at lower latitudes tend to have precipitation patterns more akin to Mediterranean climates, with dry summers, relatively wet winters, and even wetter springs and autumns.
Cold semi-arid climates are most commonly found in central Asia and the western US, as well as the Middle East and other parts of Asia. However, they can also be found in Northern Africa, South Africa, sections of South America, sections of interior southern Australia (e.g. Kalgoorlie and Mildura), inland Spain and southeastern Portugal.
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