Deserts.
Arid
The term for regions with an extremely dry climate is "arid" or "desert." These areas typically receive very little precipitation, often less than 250 millimeters (10 inches) annually, which limits vegetation and supports primarily drought-resistant flora and fauna. Examples of arid regions include the Sahara Desert and the Atacama Desert.
Dry climates often favor the development of great dry grasslands called steppes. These regions are characterized by low rainfall levels and are home to various grasses and semi-arid vegetation.
Dry arid climates can be found in regions such as the Sahara Desert in Africa, the Atacama Desert in South America, the Arabian Desert in the Middle East, and parts of Australia. These regions typically receive very little precipitation and experience high temperatures, with sparse vegetation.
The term for regions with an extremely dry climate is "arid" or "desert." These areas receive very little precipitation, often less than 250 millimeters (10 inches) annually, leading to sparse vegetation and unique ecosystems. Deserts can be hot, like the Sahara, or cold, like the Antarctic Desert.
Arid
The term for religions that develop in extremely dry climates is often referred to as "desert religions." These religions are typically characterized by their adaptation to harsh environmental conditions and often emphasize themes of resilience, spirituality, and a deep connection to the land. Notable examples include certain practices and beliefs found in Judaism, Christianity, and Islam, which have origins in desert regions.
The Amazon River Basin has a very hot and humid climate and a tropical rain forest ecosystem. The Tierra de Fuego has a dry climate.
Arid
Deserts.
Dry climates often favor the development of great dry grasslands called steppes. These regions are characterized by low rainfall levels and are home to various grasses and semi-arid vegetation.
Dry arid climates can be found in regions such as the Sahara Desert in Africa, the Atacama Desert in South America, the Arabian Desert in the Middle East, and parts of Australia. These regions typically receive very little precipitation and experience high temperatures, with sparse vegetation.
In dry climates, rates of evaporation can exceed rates of precipitation. This occurs because the hot and arid conditions in dry climates increase evaporation, while limited moisture in the air results in lower chances of rain. This can lead to water scarcity and drought conditions in these regions.
The term for regions with an extremely dry climate is "arid" or "desert." These areas receive very little precipitation, often less than 250 millimeters (10 inches) annually, leading to sparse vegetation and unique ecosystems. Deserts can be hot, like the Sahara, or cold, like the Antarctic Desert.
Dry climate regions include arid and semiarid climates. They get less than 30 millimeters of rainfall per year.
Well, Iran is quite dry and hot. So most likely Semiarid.Wikipedia describes semi-arid as:" A semi-arid climate or steppe climate describes climatic regions that receive precipitation below potential evapotranspiration, but not extremely so. A more precise definition is given by the Köppen climate classification that 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, with semi-arid areas usually being dominated by either grasses or shrubs "
1. polar climate2. continental3.MILD4.Tropical Climates5.Dry Climates6.HighLAND Climates