The ridges are shallower, and therefore when sunlight is absorbed, there is smaller mass of water to absorb the heat.
In the deep oceans, heat is transferred more efficiently, making them colder
The oceans are colder at the poles compared to the equator. Near the poles, polar regions experience colder temperatures and often have sea ice present, while the equator receives direct sunlight and is warmer, leading to higher ocean temperatures.
Sea surface temperatures don't vary by longitude. Sea surface temperatures are influenced by ocean currents; for example, the Gulf Stream current carries warmer water north from Florida to Massachusetts, and continues across the north Atlantic. If you're a hundred miles or so straight east from the Gulf Stream, the ocean temperature will be substantially cooler.
The lower oxygen levels in ocean water near the equator compared to higher latitudes are primarily due to warmer temperatures, which reduce the solubility of oxygen in water. Additionally, the high productivity of equatorial waters can lead to increased respiration and decomposition, consuming oxygen. The stratification of water layers in warmer regions also limits the mixing that would bring oxygen-rich surface water to deeper layers.
Ocean temperature varies with location and season. This variation is influenced by factors such as latitude, proximity to land, ocean currents, and solar radiation. Warmer temperatures are typically found near the equator, while cooler temperatures are found at higher latitudes and during winter months.
Because of the spinning of the Earth, wind and ocean currents closest to the equator will travel straighter. Wind and ocean currents further from the equator will deflect away from the equator.Ê
The size, and how close to the equator they are.
The world would typically have higher temperatures near the equator due to the more direct angle of the sun's rays. This leads to increased heating of the Earth's surface in those regions. Additionally, factors such as ocean currents and surrounding geography can also influence temperatures.
The oceans are colder at the poles compared to the equator. Near the poles, polar regions experience colder temperatures and often have sea ice present, while the equator receives direct sunlight and is warmer, leading to higher ocean temperatures.
The greatest amount of solar energy reaches the surface of the ocean near the equator. This is because the sun's rays are more direct at the equator, resulting in higher solar intensity. Additionally, the equatorial regions generally experience less cloud cover, allowing more sunlight to reach the surface of the ocean.
El Niño
Temperatures in the ocean vary on the location, depending on how far or close it is to the equator.
Sea surface temperatures don't vary by longitude. Sea surface temperatures are influenced by ocean currents; for example, the Gulf Stream current carries warmer water north from Florida to Massachusetts, and continues across the north Atlantic. If you're a hundred miles or so straight east from the Gulf Stream, the ocean temperature will be substantially cooler.
Ocean temperatures vary over the surface of the Earth due to a combination of factors, including latitude, proximity to land masses, ocean currents, and atmospheric conditions. Generally, temperatures are warmer near the equator and cooler towards the poles. Ocean currents can transport warmer or cooler water to different regions, impacting local temperatures. Additionally, coastal areas may experience more variability in temperature due to interactions with the atmosphere and land.
the surface of the ocean
El Niño
The southeast has warmer temperatures than the Northeast and Midwest because it is closer to the equator, which receives more direct sunlight throughout the year. Additionally, the southeast has a more humid climate due to its proximity to the Gulf of Mexico and Atlantic Ocean, which can contribute to higher temperatures.
the equator