Eastern Africa has more deserts than Western Africa, which has many more savannahs, and Southern Africa also has more deserts than Western Africa
Britain enjoys a milder climate than southern Alberta primarily due to the influence of the North Atlantic Drift, a warm ocean current that moderates temperatures. This current helps keep Britain's winters relatively mild and summers cooler compared to southern Alberta, which experiences a continental climate with more extreme temperature fluctuations. Additionally, Britain's maritime climate leads to increased precipitation and less seasonal variation, while southern Alberta's location inland results in drier conditions and greater temperature extremes.
The climate for the USA differs from region to region. There is a Mediterranean climate on the West Coast, a continental climate in the Eastern USA, a humid subtropical climate in the Southern USA, a subarctic climate in Alaska, a tropical climate in Hawaii and southern Florida, and a semiarid/desert climate in the Western USA.
Eastern Germany's climate differs from western Germany's primarily due to geographical factors and prevailing weather patterns. Eastern regions experience a more continental climate, characterized by colder winters and hotter summers, as they are further from the moderating influence of the Atlantic Ocean. In contrast, western Germany benefits from a maritime climate, leading to milder temperatures and more precipitation throughout the year. These differences are influenced by topography, proximity to the ocean, and varying wind patterns.
The North Atlantic Current is one cool ocean current that affects the climate of Iceland. This warm, swift current brings relatively mild temperatures to Iceland, making its climate milder than other regions at similar latitudes.
The northern and southern portions of the world are primarily dominated by polar climate zones. The Arctic region in the north features a polar climate characterized by extremely cold temperatures and minimal precipitation. In the south, the Antarctic region also exhibits a polar climate, with similar conditions of frigid temperatures and ice-covered landscapes. These polar zones are flanked by subpolar regions, which experience milder weather but still have significant cold temperatures.
The massive heat sink known as the ocean.
The milder climate and better opportunities to feed are the most obvious reasons.
The climate in Africa varies widely, with some regions experiencing tropical, desert, arid, Mediterranean, and subtropical climates. Generally, Africa is known for its hot temperatures, especially in central and northern regions, while southern Africa can have a milder or cooler climate. Rainfall patterns also differ, with some areas experiencing heavy rain and others being very dry. Overall, Africa's climate diversity is influenced by factors like latitude, altitude, proximity to water bodies, and prevailing wind patterns.
The climate for the USA differs from region to region. There is a Mediterranean climate on the West Coast, a continental climate in the Eastern USA, a humid subtropical climate in the Southern USA, a subarctic climate in Alaska, a tropical climate in Hawaii and southern Florida, and a semiarid/desert climate in the Western USA.
Russia features a diverse range of climate types, primarily including subarctic, continental, polar, and temperate climates. The subarctic climate is prevalent in Siberia, characterized by long, harsh winters and short summers. The continental climate dominates in central and eastern Russia, with significant temperature variations between seasons. In the far north, the polar climate is found, marked by extremely cold temperatures, while the temperate climate exists in the southern regions, featuring milder winters and warmer summers.
Eastern Germany's climate differs from western Germany's primarily due to geographical factors and prevailing weather patterns. Eastern regions experience a more continental climate, characterized by colder winters and hotter summers, as they are further from the moderating influence of the Atlantic Ocean. In contrast, western Germany benefits from a maritime climate, leading to milder temperatures and more precipitation throughout the year. These differences are influenced by topography, proximity to the ocean, and varying wind patterns.
Isle of Wight climate is milder than most places in England.
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A marine climate will generally be cooler in summer and milder in winter and a continental climate will be hotter in summer and colder in winter.
The climate in the 13 colonies varied from the cold winters in the northern colonies to the milder climate in the southern colonies. The soil was generally fertile and suitable for agriculture, with regions like New England having rocky soil and the southern colonies having rich, fertile soil ideal for cash crops like tobacco and cotton.
Crimea has a warmer climate compared to Kiev. Being a region located along the Black Sea, Crimea experiences milder winters and hotter summers, while Kiev has a continental climate with colder winters and milder summers.
The western US tends to be drier with more extreme variations in temperature, due to its proximity to desert regions and mountain ranges. The eastern US has a milder climate with more consistent precipitation, influenced by its proximity to the Atlantic Ocean and Gulf of Mexico. These factors result in differences in weather patterns and vegetation between the two regions.