Antarctica Report - The Location And Purpose Of Mawson Station

Authors Avatar by jackbardsleystudentscotchwaedu (student)

 

             Emperor penguins during summer (Gaidos, 2009)

  Arial photo of Mawson Station (Australian Antarctic

                                    Division, 2012)

       Emperor penguins swimming near Antarctica (Wienecke, 2011)

Contents        

 Report……………………………….……………………….......  Pg.  3-8

Introduction……………………………………………........... Pg. 3

Climate…………………...…………………………………..... Pg. 3-5

Location And Purpose Of Mawson Station……………...  Pg. 6-8

Adaptions To The Antarctic Environment……………….  Pg. 8-10

  • Human Adaption…………………………………...………………...     Pg. 8-9

  • Animal Adaption……………………………...………………………   Pg. 9-10

Conclusion……………………………………………………    Pg. 10

     

References……………………………………………………… Pg. 11

Appendix…………………………………………………………Pg. 12-17

   

 

Antarctica lit up by a colourful aura (Maugans Corporation , 2012)

               

Antarctica Report

Introduction:

The great icy continent of Antarctica is located at the south-most point on Earth and in the heart of the Antarctic Circle, referred to as the ice-cold desert.  Antarctica covers the entire land and water region south of the latitude 600 S with no defined longitude, the continent spans around the entire Antarctic Circle. In reference to Australia, the eastern half of Antarctica ranges from a close 3,800km south of mainland Australia with Mawson Station located further west.  Due to its location, early expeditions to Antarctica were usually carried out on boat with a stop at islands along the way i.e. Macquarie Island- now one of the four main Australian research bases in Australian Territory of the Antarctic Peninsula.

 

Australia controls the largest part of Antarctica (43%) because of Sir Douglas Mawson’s expedition to Antarctica in 1929-31. During this expedition, Mawson and his team mapped majority of the Eastern coast, setting up camps along the way and eventually other Australian expeditions set up stations using these maps. Later when the Antarctic Treaty was established, this link with Antarctica and the fact that Australia was the first nation to map the eastern coast was considered, resulting in Australia’s claim to this area being granted, leaving them with majority of Antarctica.

The governing of Antarctica is unique and very different from the rest of the world. It is governed by many nations that have all claimed parts of the continent for scientific research who all are guided and bound by “The Antarctic Treaty”. “The Antarctic Treaty” was designed and created by twelve original countries (there are now 38 countries) in 1961 to provide an agreement for the future care and use of Antarctica and to avoid territorial and other disputes. The Treaty encourages international co-operation in scientific research and in recognition of Antarctica being the last remaining “wilderness” on Earth, the ‘Madrid Protocol’ was established to help the conservation of the environment and peace on Antarctica. Elements of The Antarctic Treaty include: Antarctica shall be used for peaceful purposes only (Art.1), Freedom of scientific investigation and cooperation shall continue (Art.2), Scientific observations and results from Antarctica shall be exchanged and made freely available (Art. III).

Lying at the south-most point on Earth, Antarctica is truly a unique continent, renowned for a very harsh climate and an environment that has caused both, humans and animals, to adapt to the extreme conditions. Despite minimum infrastructure, Antarctica houses various forms of extensive scientific research conducted at its numerous bases.

Climate:

Mawson’s climate is typical of much of the coast of East Antarctica where the ice caps are present at sea level.  The climate of Mawson Station can be described and categorized into four main areas: rainfall, temperatures, wind speeds and direction and mean daily averages.

One of the main features of Mawson’s climate are the extremely cold daily maximums and minimums present there through most of the year. The mean maximum temperature ranges from its hottest at about 2.60C in January to the lowest daily maximum-15.60C in the peak of winter (July, August, September). The annual mean for the daily maximum is -8.40C, around the same as the mean in March and October.

The mean daily minimums are not vey different to the daily maximums, a contrast compared to most parts of the world where the daily minimum and maximum have a greater difference. The mean daily minimum is at its highest in the month of January at -2.60C, dropping down considerably in March by almost 110C to -13.30C, marginally warmer than the annual minimum average of -14.3. Similar to the mean daily maximums, the mean minimums are at their lowest in winter, leaving a gap/difference of about 60C between the two (maximum and minimum). Although the mean temperatures around Mawson are mostly in the negatives, they are still a lot warmer and pleasant than those experienced in majority of Antarctica’s inland as the station lies near the coast and at a lower altitude of about 1,200m compared to the inland where altitudes rise up to almost 3,00m above sea level. 

Another characteristic of Mawson’s climate is the incredible winds experienced at Mawson and their high speeds. Winds around Mawson blow predominantly from the east and south, heading in a northwest direction. The mean annual wind speed is almost 40 km/h at 3pm, with some extreme speeds go past 120km/h during the year in peak winter (3pm). The maximum gust speeds exceed 140 knots frequently with the highest recorded wind gust ever in the area reaching an amazing 248.4km/h early in the morning. Wind speed are generally stronger during the winters, rising up to an average of 44km/h in August at 3pm compared to an average of 27-28km/h in December/January.

Most precipitation falls as snow in Antarctica with no significant rainfall recorded near Mawson Station. As a result of Antarctica receiving less than 50mm of rainfall per year, the Antarctic region is classified as a desert-the coldest and driest desert in the world. Snowfall occurs regularly throughout the year-mainly during late summer when the snow is still able to fall without freezing. Although this snowfall is not very significant, it still has an impact on the climate around Mawson Station.

The lowest temperatures at Mawson vary greatly as the seasons change. During the seasons of autumn and spring, the lowest ever recorded temperatures for each month (during these two seasons) have been very similar. The lowest temperatures of March, April and May all range within the late twenties to early thirties, almost identical to those of September, October and early November. Where as, the lowest ever temperatures in winter and summer are in great contrast, as the lowest during summer goes down to a less extreme -17.30C in February compared to freezing -360C in August.

The reason for Antarctica’s very cold climate and its frequent change of size is the concept of the Earth’s revolution. The Earth is constantly rotating around an axis that runs through the north and South Pole at an angle of incidence (leaving the Earth always at a tilt of 23.50), completing one rotation every 24 hours. The Earths rotation is the reason that day and night are experienced, as when a part of the world is facing towards the Sun, it would be day, and when it rotates around to be away from the Sun, it becomes night. While the Earth is rotating on its axis (completing a rotation every 24 hours), it is in constant revolution around the Sun (completing a revolution every 365 days).

As the Earth is always tilted the same way, the stage at which the Earth is at during its revolution determines the concentration and strength of the rays hitting the particular area. For example, if it is December 21 in the southern hemisphere the angle of incidence will have this part of the Earth closer to the Sun/tilted towards it causing the Sun’s ray to be concentrated at a smaller area and thus being stronger and creating more heat. This is because; during summer the Sun is directly above the Earth due to the tilt. As the equator is in no hemisphere, the angle of the rays is the same throughout the year, creating the same season for 365 days. Where as, the poles, which are located at top of the northern hemisphere and bottom of the southern hemisphere, have two completely different seasons. During summer they rotate around the axis but are always facing towards the Sun, thus having sunlight for almost 24 hours per day. However, during winter, the poles- in this case the south pole- is tilted away from the Sun and when rotating on the tilted axis, it remains away from Sun for most of the time, thus having no sunlight. This process/revolution continues for the whole year, in which the South Pole has experienced both summer and winter. Because of this reason and that it is located around the South Pole, Antarctica experiences these extreme amounts of daylight and darkness. As a result of these extreme seasons, a huge amount of sea ice is formed during winter, as the temperature gets extremely cold, quickly melting as summer approaches and the temperature rises above freezing point. If Antarctica were located near the equator, this effect would not occur as firstly, the temperatures would not be as low because the suns ray’s are stronger there because of the angle of incidence, but also the change in seasons would not be as extreme with the hours of daylight barely varying throughout the year.

Join now!

Mawson Station:

Location: Mawson is a particularly favourable location for a station, with excellent access to the hinterland/open inland areas and surrounding coastal waters. It is also located near a harbour sheltered from the main body of the ocean and with a large depth and mouth not too narrow, during the ice-free period usually experienced in February, a ship may anchor within 100 metres of the station. Barges carrying the cargo would take only a few minutes to travel from the ship to station as it is located right on the shore. There is also a “magnetic quiet area” for research ...

This is a preview of the whole essay