The modern zones we recognize today can be loosely related to the ancient Greek zones of torrid, temperate, and frigid. However, it is important to note that there are some differences in terminology and classification.
1. Torrid Zone: The ancient Greek torrid zone refers to the hot, tropical regions around the equator. In modern terms, this zone can be divided into two main classifications: the Tropical Hot Zone and the Tropical Dry Zone. The modern tropical hot zone aligns with the ancient Greek torrid zone, as it represents the hot, humid areas closer to the equator. The modern tropical dry zone encompasses areas with hot temperatures but less rainfall, which can be related to the drier parts of the ancient torrid zone.
2. Temperate Zone: The ancient Greek temperate zone refers to the areas with moderate climate, located between the torrid and frigid zones. In modern classification, the temperate zone is divided into the Midlatitude Mild and Midlatitude Severe zones. The midlatitude mild zone generally corresponds to the ancient Greek temperate zone, representing areas with moderate temperatures and distinct seasons. On the other hand, the midlatitude severe zone includes regions with more extreme seasonal variations, such as areas with hot summers and cold winters.
3. Frigid Zone: The ancient Greek frigid zone represents the cold polar regions. In modern terms, the polar zone aligns with the ancient Greek frigid zone, encompassing the areas near the North and South Poles with extremely cold temperatures.
While there is a broad correlation between the ancient Greek zones and the modern ones, it is important to note that the ancient Greek classification was based on a general understanding of the world without precise scientific measurements. The modern classification takes into account more accurate and detailed scientific data, resulting in more specific delineations of climatic zones.