It is known as the Gulf Stream.
mild
No, the Humboldt Current and El Niño currents are not the same. The Humboldt Current is a cold ocean current that flows north along the western coast of South America, while El Niño is a climate phenomenon characterized by the warming of sea surface temperatures in the central and eastern tropical Pacific Ocean which can disrupt weather patterns globally.
The Benguela Current, flowing northward along the southwestern coast of Africa, significantly influences the climate of western Africa by bringing cool, nutrient-rich waters that support marine life. This cooling effect helps moderate coastal temperatures and contributes to arid conditions in regions such as Namibia and southern Angola. Additionally, the current impacts local weather patterns, reducing rainfall and fostering desert-like environments in adjacent areas. Overall, it plays a crucial role in shaping the ecological and climatic characteristics of the region.
A warm ocean current flowing north from the gulf of Mexico, along the east coast of the U.S. , to an area off the southeast coast of Newfoundland, where it becomes the western terminus of the north Atlantic current.
The Gulf Stream helps to moderate the climate on the western coast of Norway, creating milder winters compared to other regions at similar latitudes. This warm ocean current brings in relatively warm water from the Gulf of Mexico, which helps to warm the air above it and maintain a more temperate climate in Norway.
The Gulf Stream.
The Gulf Stream?
The gulf stream - it carries warmth towards northern Europe.
The Alaska Current is a warm-water eddy current resulting from the northward diversion of a portion of the North Pacific Current when that current meets the west coast of the North American continent. It is warmer than most sub-Arctic Pacific water with temperatures above 39° F (4° C). As such, it has a warming effect on the climate of British Colombia and southern Alaska
The Alaska Current is a warm-water eddy current resulting from the northward diversion of a portion of the North Pacific Current when that current meets the west coast of the North American continent. It is warmer than most sub-Arctic Pacific water with temperatures above 39° F (4° C). As such, it has a warming effect on the climate of British Colombia and southern Alaska
mild
The ocean current flowing southward along the western coast of the United States to northern Baja California is called the California Current.
"Climate Change" and "Global Warming" are not the same, though related. Global Warming causes Climate Change. With Global Warming we understand the warming of the earth's global temperature. That warming has in turn an effect on the earth's global climate and on more localized climates (like the climate of England or Western US).
Western Europe's moderate climate is influenced by the warming effects of the North Atlantic Current (part of the Gulf Stream), which brings warm waters from the Gulf of Mexico. This helps to moderate temperatures and create milder winters compared to other regions at similar latitudes. Additionally, the presence of mountain ranges like the Alps and the Pyrenees help to block cold air masses from moving into the region, further stabilizing the climate.
Receives some warming effects of the north in the summer.
No, the Humboldt Current and El Niño currents are not the same. The Humboldt Current is a cold ocean current that flows north along the western coast of South America, while El Niño is a climate phenomenon characterized by the warming of sea surface temperatures in the central and eastern tropical Pacific Ocean which can disrupt weather patterns globally.
The North Atlantic Current is a vast, slow moving warm current. It is created from the Gulf Stream and the Labrador Current joining at southern Greenland, which creates the widening and slowing of the Gulf Stream. The North Atlantic Current splits near western Europe, one part creating the warm Norway Current flowing northward along the coast of Norway and the other creating the cold Canary Current deflecting southward, eventually warming and rejoining the North Equatorial Current.