Because water absorbs heat keeping it from making it hotter and then over the course of inter releases it keeping it from getting cold. In other words the farther inland you go the more extreme temperatures get. This is why places like New Zealand don't get much snow even though they are far from the equator and why Siberia is the coldest place on earth. Its also why places such as Midwest America get much colder than, say Britain, the western coast and most of the eastern coast(excluding parts more north like New York and Maine)
Yes, the seasonal shift of isotherms is greater over continents than over oceans. This is because land heats up and cools down faster than water due to differences in heat capacity. As a result, the temperature difference between summer and winter is more pronounced over continents, leading to larger shifts in isotherms.
Isotherms shift during the seasons of the year because of the varying amount of solar radiation received on Earth's surface due to the tilt of its axis. In winter, lower sun angles and shorter days result in less heating, causing isotherms to shift towards the equator. In summer, higher sun angles and longer days lead to more heating, causing isotherms to shift towards the poles.
Continents warm up and cool down faster than oceans due to differences in heat capacity. During summer, continents absorb more heat from the sun compared to oceans but also lose heat more quickly. This leads to higher temperatures on continents than in adjacent ocean waters.
The yearly total precipitation over the oceans is greater than over continents because oceans cover more of the Earth's surface and therefore have a larger area from which to receive precipitation. Additionally, the oceans are able to retain heat better than land, leading to more evaporation and subsequent precipitation. Ocean currents also play a role in transporting moisture to different regions, contributing to higher precipitation levels over oceans.
The pressure over continents changes with the seasons due to variations in temperature. During the summer, continents tend to warm up more quickly than the oceans, creating a low-pressure system as warm air rises. In winter, continents cool down faster than oceans, leading to a high-pressure system as cold air sinks.
Yes, the seasonal shift of isotherms is greater over continents than over oceans. This is because land heats up and cools down faster than water due to differences in heat capacity. As a result, the temperature difference between summer and winter is more pronounced over continents, leading to larger shifts in isotherms.
Continents by a couple
Isotherms shift during the seasons of the year because of the varying amount of solar radiation received on Earth's surface due to the tilt of its axis. In winter, lower sun angles and shorter days result in less heating, causing isotherms to shift towards the equator. In summer, higher sun angles and longer days lead to more heating, causing isotherms to shift towards the poles.
Because we tend to spend more time on the continents than in the oceans.
Isotherms tend to be more irregular in the southern hemisphere due to the distribution of land masses and oceans. The presence of large oceanic bodies can lead to more variation in temperature patterns, resulting in more irregular isotherms. Additionally, the absence of large land masses to stabilize temperatures can also contribute to this irregularity.
All of them. You listed the four oceans; all of the continents border one or more of the oceans.
Isotherms, which are lines connecting areas with the same average temperature, generally exhibit a greater seasonal shift over land compared to the ocean. This is because land heats up and cools down more quickly than the ocean due to differences in heat capacity and heat transfer mechanisms. Therefore, the temperature variation on land between seasons is usually more pronounced than that over the ocean.
Asia and South America are not oceans, they are continents.
Continents warm up and cool down faster than oceans due to differences in heat capacity. During summer, continents absorb more heat from the sun compared to oceans but also lose heat more quickly. This leads to higher temperatures on continents than in adjacent ocean waters.
The Robinson projection splits the Earth's oceans apart in order to more accurately represent the sizes and shapes of the continents. This projection is a compromise projection that tries to balance the accurate representation of both landmasses and oceans.
Continents generally heat and cool faster than oceans due to differences in their heat capacity. Oceans have a higher heat capacity because water can store more heat than land, so they heat up and cool down more slowly. This is why coastal areas typically experience more moderate temperatures compared to inland regions.
The yearly total precipitation over the oceans is greater than over continents because oceans cover more of the Earth's surface and therefore have a larger area from which to receive precipitation. Additionally, the oceans are able to retain heat better than land, leading to more evaporation and subsequent precipitation. Ocean currents also play a role in transporting moisture to different regions, contributing to higher precipitation levels over oceans.