Monday, 20 January 2014

Group Blog #2 - Group A

Distinguish between two chosen hazards in terms of their spatial extent, predictability, frequency, magnitude, duration, speed of onset and effects. [10 marks]


In a world constantly changing, natural hazards are common and sometimes inevitable. There are numerous kinds of hazards. Namely, earthquakes, volcanic eruptions, tsunamis, hurricanes, typhoons, and drought. The chief focus of this essay is to distinguish between earthquakes and typhoons/hurricanes. 

Spatial Extent:

Earthquakes and typhoons are very different in that they are two kinds of extremes. Earthquakes occur within the earth, whilst typhoons are occur in the sky. Earthquakes are caused by the movement of tectonic plates, therefore they happen mostly along tectonic plate boundaries. 

Figure 1: map of tectonic plates

Figure 1 above shows the tectonic plates. A recurring location for earthquakes is Japan, which lies directly on the boundary between the Eurasian Plate and the Philippine Plate.

Typhoons on the other hand, these occur in low pressure systems above tropical waters. Eastern and Southeast Asian countries, such as Philippines, India, and China experience numerous typhoons annually. 

Figure 2: spatial distribution of hurricanes/typhoons
As evident in figure 2, typhoons are abundant along the tropics, as well as in northern Australia.

Predictability

Earthquakes and Typhoons are distinct in that earthquakes are difficult to predict, because the only definite way of predicting a quake is moments before it strikes, through foreshocks. On the other hand, typhoons can be more easily tracked and predicted. This is because typhoons form a large mass of wind, rain, and clouds that can easily be seen by a satellite.

Frequency & Magnitude

Earthquakes happen frequently, but the magnitude differs. Generally speaking, the greater the magnitude, the less frequent the quake. A magnitude of less than 2 on the Richter scale happen several million times in one year, while a magnitude of 9 or greater will occur once in 10-50 years. For example, during the 2010 Christchurch earthquake, there were 12,911 quakes within 24 hours. 

Typhoons as a whole do not occur as often as earthquakes, stronger typhoons are much more common than stronger earthquakes. Most typhoons typically occur in the months of June and July, and become less frequent in the months of January and February. The reason for the large occurrence in June/July is because of the warmer waters. Stats show that between 1959 and 2011, there was an average of 5.6 typhoons in the month of August.

Figure 3:Satellite image of typhoon Yolanda approaching the Philippines


Speed of Onset

An earthquake typically lasts only a few seconds, however, the aftershocks can continue for months after the initial quake. For example, in Japan, the earthquake that happened in April of 2011, had aftershocks as far as December 2012. Typhoons, typically last longer than an earthquake. They can last from a few hours and a couple of days, depending on the speed and velocity. 

Effects 

Both earthquakes and typhoons can potentially cause a range of damages, from minimal damage to catastrophic. 

This can be seen through earthquakes. There are thousands of quakes a day and very little are felt on the surface. Conversely, earthquakes have the potential to cause massive destruction. An example is the 9.0 magnitude earthquake in Japan. It caused a tsunami with 13,355 fatalities. 

Figure 4: Damage caused by Christchurch earthquake

Typhoons bring a lot of rain and wind to a particular area. Hurricane Frances in 2004 only caused 6 casualties, wherein Typhoon Yolanda in 2013, which was recorded as the strongest typhoon to ever hit landfall, caused 5,260 casualties. Asides from lives being taken, the livelihood of people can be destroyed. In areas such as the Philippines, during the strongest typhoons, farmers lose their crops and fishermen suffer from a decline in fish yields. The extent of these damages can be seen globally, and do not only occur in LEDC's.

Figure 5: Damage caused by typhoon Yolanda
In conclusion, earthquakes and typhoons differ greatly in characteristics, predictability, and spatial distribution, however, they are similar in that they can cause catastrophic damages to the infrastructure of an area as well as destroying the livelihoods of numerous people, especially in LEDC's. Natural hazards are, as they are called, natural. These are often inevitable and the best way to approach these hazards is to be prepared. 


Sunday, 19 January 2014

Group Blog #1 - Individual

Explain the characteristics and spatial distribution of the following hazards using at least two specific examples. [10 marks]

It is important to be aware of hazards, especially the characteristics and spatial distribution. Knowing about hazards can help prevent future repetition, by educating the people. Characteristics are essentially the facts, whilst the spatial distribution is the location of the hazard and the area it affects. The characteristics and spatial distributions will be discussed in light of two disastrous earthquakes: the 2010 Christchurch Earthquake and the 2011 Japan Earthquake.
The Christchurch Earthquake happened on September 4, 2010 in the city of Christchurch, New Zealand. Christchurch is New Zealand’s second largest city, with approximately 386,000 people (BBC). Fortunately, there were no direct casualties, and only a few injured people (BBC). It is arguable that the reason behind the minimal casualties is because the quake took place at 4am, where there were little to no people on the streets.
Figure 1: Before and after image of a building in Christchurch.
The quake scored a 7.1 on the Richter scale, and lasted around 40 seconds (TVNZ). On the same day, there were 12,911 after shocks, not all of which were felt on the surface (Nicholls). The quake was surprisingly not predictable, because though New Zealand lies in the boundary of the Australian the Pacific plates, the fault line runs along the southern alps, which is a considerable distance from Christchurch. Experts only discovered and declared a fault line under the Canterbury plains – the area of relatively flat land between Christchurch and the Southern Alps – upon the event of the earthquake (BBC & Nicholls). Moreover, the epicenter is in the Canterbury plains, some 35kilometres away from the city centre, and is only about 12kilometres deep.
Figure 2: 7.1 magnitude earthquake's epicentre and area of influence. Christchurch is to the east, and the Southern Alps is to the west.
On the other hand, the 2011 Earthquake that hit eastern Japan, near the city of Sendai, was notably more disastrous. The quake affected 2,100km of coastline, including the city of Tokyo. This quake was particularly damaging because it caused a 7metre tsunami, which hit Hawaii within 24 hours. The tsunami was so large in scale that there were warnings along the west coast of the United States, Canada, and South America. Additionally, a few nuclear power plants were affected, which consequently affected some surrounding residential areas, hundreds of kilometres away from the epicenter (Huffington Post).
Figure 3: Map showing the epicentre, neighbouring city of Sendai,and the eastern coast that was affected.

The quake was reported to have a magnitude of 8.9 on the Richter scale, with over 50 after shocks, some of which had a magnitude of over 6.0 on the Richter scale. Unlike the Christchurch Earthquakes, this quake was somewhat predictable, because Japan is a country that has experienced its share of destructive earthquakes, such as the 1996 earthquake in Kobe that caused over 100,000 casualties (Huffington Post).There is no denial that earthquakes, as well as other natural disasters, are inevitable. However, being aware of the causes and vulnerability of a certain place to certain disasters can aid in future planning, in order to avoid repetition and to perhaps fix the catastrophic damage that is still visible from these quakes. It is far more beneficial for people to learn about these hazards, so that they can invest in proper infrastructure and safety methods for the future.




Citations:
"Magnitude 7.1 Earthquake Hits Chch." TVNZ. N.p., 4 Sept. 2010. Web. 18 Jan. 2014. <http://tvnz.co.nz/national-news/magnitude-7-1-earthquake-hits-chch-3759865>.
Nicholls, Paul. "Christchurch Quake Map." Christchurch Quake Map. University of Canterbury's Digital Group, n.d. Web. 18 Jan. 2014. <http://www.christchurchquakemap.co.nz/>.
Snyder, Whitney. "Japan Earthquake 2011: 8.9 Magnitude Earthquake Hits, 30-Foot Tsunami Triggered." The Huffington Post. TheHuffingtonPost.com, 11 Mar. 2011. Web. 18 Jan. 2014. 
<http://www.huffingtonpost.com/2011/03/11/japan-earthquake-tsunami_n_834380.html>.
"Strong Earthquake Rocks New Zealand's South Island." BBC News. BBC, 3 Sept. 2010. Web. 18 Jan. 2014. <http://www.bbc.co.uk/news/world-asia-pacific-11183685>.
Figure 1: https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj978UNoZqnAEHh328pTVA24bEH-Wqa0bEClEDZK4yxSSDb_VulqiGAxcQqoxMB6c3Tv_iztiIc3cTukQ12hohPpiEey_HzdZm2mvuu1TdsrWEJMS-Ll5Hhsa_lhRdKiL9SCfFBRQfYvEi4/s1600/11PyneGould.jpg

Figure 2: http://www.christchurchquakemap.co.nz/largest

Figure 3: http://www3.pictures.zimbio.com/mp/stTwmvCmbXJl.jpg