Seasons change due to the tilt of the Earth which is 23.5 degrees as it orbits around the sun. When the Northern Hemisphere is tilted towards the sun, it is Summer for that part of earth and winter for the Southern Hemisphere because of the indirect sunlight. Althpugh they both still recieve some sunlight during summer but they do not reach hot temperatures. Six months later when the Earth is on the other side of the sun it would be the opposite with the Southern Hemisphere pointing towards the sun and the Northern facing away. When the earth is midway through its orbit, both hemispheres receive the same amount of rays making it spring and autnm. The North and South Pole always remain cold because of indirect sunlight. Only a small part
3. Based on your answers, why is it warmer in summer than in winter? It is warmer in the summer then in the winter because the Earth’s tilt is
Climate is closely associated with the seasons, but do you know what causes the seasons? Log on to the website
Tropic latitudes, alongside polar areas, would have a more dramatic change in daylight periods throughout their seasons because of their varying solar angles throughout the months while completing a single orbit. The equatorial region experiences minimal beam spreading and depletion of solar radiation due to the shorter path it travels through the
Because the experiment is only take place in 1 hour the season will not affect the results. If I had a whole year to carry this experiment out I would do the experiment throughout different seasons to see what affect the seasons has on the results.
The idea that Harvard graduates had that the earth revolves around the sun at different lengths is a common misconception that can be proven inaccurate. The seasons occur when parts of the Earth receive more or limited amounts of sunlight during the year. This is caused by the Earth's axis always pointing to the North Star instead of moving while revolving around the sun. This causes both the Northern and Southern hemisphere to receive different amounts of sunlight throughout the year. An example of this is the differences between the two cities Dublin, Ireland, and Punta Arenas, Chile.the Latitude of Dublin is 53.3498 degrees north, while Punta Arenas has the latitude of 53.1638 degrees south. This means that both places experience opposite
el nino is a warm band of water that periodically develops in the Pacific Ocean near the equator off western South America. El Niño—Spanish for “the child” because it often occurs around Christmas—occurs about once every two to seven years. El Niño can affect the weather in large parts of Asia, Africa, Indonesia, and North and South America, causing both floods and droughts. An El Niño event is often followed by a band of colder than normal ocean waters called La Niña, which is Spanish for “the girl.” La Niña produces the opposite weather conditions. Both of these phenomena cause changes in air pressure in the western Pacific. Together these two events are known as ENSO, or El Niño–Southern
It would still be warm at the tropical zones and cold at both of the poles. The seasons that we experience now are caused by the tilt. For instance, in the summer, the Northern Hemisphere is tilted towards the sun, while the Southern Hemisphere is tilted away from the direct sunlight (“Earth”, 2016). The direct sunlight provides the Northern Hemisphere the maximum amount of direct sunlight. For places in the Southern Hemisphere, such as Australia, it provides the least amount of direct sunlight, which is why they experience winter at this time. When we have winter, it is the exact
Temperature contrast between the equator and the Arctic region is greatest in the winter. Temperatures near or at the equator only change a few degrees between winter and summer while the Arctic region changes drastically up to 40 degrees between the seasons.
of the Arctic as well as the long summer days of Antarctica.” Another reason I believe this is because they have two summers!
The Earth is tilted on an axis with the northern point of our planet tilted at 23.5 degrees toward the sun as we orbit it. The Earth also rotates on this tilted axis, which is how we get our days. The reason that Ohio gets warmer in the summer is because as the Earth rotates the sun (one rotation around the sun equals one year), different sections of the Earth "take turns," as you might say, being "closer" to the sun. As the Earth passes by one side of the sun, the northern hemisphere will be tilted towards the sun in the same way that the northern hemisphere would be tilted away from the sun when the Earth passes by the opposite side. So, it is warmer in the summer because the summer time is when the northern hemisphere is tilted closer to
In this article it talked about the climate changes in latin america. Some of this changes include, the sea level rise, the rainfall pattern, melting glaciers, agricultural regions, and the development of diseases. All of these changes are happening in Latin America. It also talk about what latin america has.
The average person believes that seasons are a result of the sun 's rotation around the Earth, but there is much more involved than what people assume. The Earth 's seasons are affected by many different factors such as the influence of different hemispheres, rotation of the sun, and greenhouse gases. They will also continue to change over time. The climate has a huge effect on the seasons and the population. The Earth 's seasons end up having a ripple effect on people, plants, animals, and agriculture that helps feed the world. Climate effects people on a regular basis in a way they do not realize.
The El Nino Southern Oscillation is a large scale circulation of atmospheric and oceanic interactions. It is a natural climate phenomenon where the tropical Pacific Ocean experiences higher than normal ocean temperature. The opposite, La Nina, refers to the unusual cooler than normal sea surface temperatures. It gained its name “the Christ child” in Spanish (“the girl” for La Nina) because the characteristic is most obvious around Christmas alone the western coast of South America where it was first discovered.
The processes occurring in the upper ocean are important for interpreting the global climate and its variability. The upper ocean is often referred to as the ocean mixed layer (ML). It is a quasi-homogeneous layer of oceanic tracers regulated by turbulence due to air-sea exchanges of heat and momentum fluxes. The thickness of the ML modulates its heat capacity and controls the evolution of sea surface temperature (SST), which is important for understanding climate dynamics. Therefore, the mean state and seasonal cycle of ocean mixed layer depth (MLD) and the relative roles of net heat flux (NHF), wind-stress and freshwater flux on the ML require to be explored over the global ocean. Insufficient attention has been given to the role of