Welcome!

Why hello there and welcome to my Geography blog. I'm an A-level student from Somerset studying Environmental Science, Geography and Archaeology. I should probably explain how this blog has come about. During my first lesson of the new year my teacher exclaimed that I should start a “What I learnt this week…” blog. I thought this would actually be a good idea to help for revision and “consolidate my learning” which is what the teachers always tell me to do and it might (hopefully) help other people doing geography as well. So this is my geography blog.

There are two of us!

So i am a geography geek and got added so i can blog too. what can i say, i love it absolutely love it! i'm not really that clever (that's a lie she is!) but it doesnt stop a love i have for the subject, i also study environmental science and geology.

My portrait photo should reflect what topic I'm studying at the time. If I remember to change it... If you have any questions or want to talk to us about anything Earth Sciences related please don't hesitate to ask!

Wednesday, 30 March 2011

The alternative geography lesson

During what would have been during todays lesson we were scrambling around a cave. A cave covered in an inch of ice, which is very slippery and very scary.
Apparently it's not supposed to be that icy and our Icelandic tour guide kept telling us it's only a "little slippery".  He was lying, it was a death trap in there. The only way forwards was to bum shuffle-fact! But to be honest it was one of the most exciting things we haver ever done and very very enjoyable. The fact that it was so icy made it more exciting and made us group together more as a team. That led us to sing most of Bohemian Rhapsody, the Bed Intruder Song and (to James' disgust) some Take That (which I refuse to link to). Eventually we made it through the cave after some tricky climbing only to be faced we a crawl through the smallest gap imaginable up some ungrippable snow...


We were actually caving through a lava tube which formed about 4000 years ago. This formed by basalt lava flows cooling on the top and sides providing insulation for the centre which can remain active for several years. Lava tubes on Hawaii are still active and they work for a long time. Lavascicles are formed when lava cools and drips down from the ceiling (just like water does).
Vicky looking as glamorous as always...

Sunday, 13 March 2011

Temperate Climates

Cool Temperate Western Maritime Climates don't you just love 'em? Well if you don't then, unless you're planning on emigration, you need to get used to them.

So where are they found?

- Well between 40 and 60 degrees North/South constitutes a temperate climate
- And being on the Western edge of a continent constitutes a maritime climate
- What determines how far inland the climate extends is based upon the relief of the land

There are three types of rainfall: - Orographic Rainfall
                                                         - Convectional Rainfall
                                                         - Frontal Rainfall

So what other countries are remarkably lucky to share the same climate as the wondrous UK?

- South West New Zealand
- Chile, the Andes block the climate from extending any further within the country
- Canada, Vancouver - the Rockies block the climate from extending any further
- Western Europe, quite a few countries share our climate because the climate doesn't get blocked until the Alps

What does a Cool Temperate Western Maritime Climate mean?

- Weather is changeable with no marked seasonal differences
- Plenty of cloud and precipitation all year round
- Extremes of temperature are rare
- Low annual temperature range
- Fairly strong winds
- Warm summers
- Mild winters

- Maritime climates are unique as they are unusual to what we'd expect on similar lines of latitude. For example the UK are on a similar latitude to Moscow yet we experience a vastly different climate.
       - The reason for this is due to the high specific heat capacity of water. Water takes longer to heat up and cool down than land, this means that summers are cooler than expected and winters are milder.


Any questions?

Thursday, 10 March 2011

Belfast

So to steal a small concept from Cryss

Number of exam results received today: 1
Number of results I was pissed off with: 1
Number of times I punched the wall: 15+

Clearly this blog didn't help me as much as I would have liked for the Belfast exam however the purpose of the blog wasn't purely to help me get higher grades but to hopefully help other people understand. So what I'd like to know is whether this blog is worth it, if it actually helps people understand and they find it useful then I'll carry on writing the blog. If people don't find it useful then I don't think there's much point in me carrying it on.

Basically if this blog is helping, speak now. If it's not then it'll probably disappear.

James

Thursday, 3 March 2011

The Atmosphere

I am unbelievably bored, have nothing else to do and seeing as the blog hasn't been updated in a while I thought I'd explain the atmosphere in greater detail. They're in stratigraphical (is that a word?) order starting from sea level.



The Troposphere

Oh what a glorious place it is... This is the first layer of our atmosphere and it is heated via infrared radiation being radiated from the Earth, this means that as altitude increases temperature falls. Atmospheric pressure also decreases with altitude, there's a simple reason for this. The higher you go the less there is above you so the pressure decreases. Wind speeds increase with altitude in the troposphere as at higher altitudes there is less to act as a wind break.

Stratosphere

Once you get through the troposphere everything starts getting a bit warmer until temperatures reach a toasty -3 degrees Celsius. The reason the temperatures increase with altitude is because the stratosphere is heated by the absorption of  UV radiation by Ozone (so from above, not below).
When ozone absorbs UV it gets split up into Diatomic Oxygen and Atomic Oxygen, in the normal process this would then bond again to form Ozone. The ozone layer should remain in dynamic equilibrium (constantly changing, but overall staying the same), however when CFCs are emitted into the atmosphere they also get broken down. The Chlorine atom then bonds with an Atomic oxygen atom to form ClO preventing the atomic oxygen bonding with diatomic oxygen to replenish the ozone layer. So in reality CFCs don't destroy the ozone layer but rather prevent it from replenishing itself.

Mesosphere
Not much really goes on here to be fair, temperature decreases with altitude for reasons I can't accurately find out but I do know that the mesopause house the coldest temperature on Earth. The only other thing interesting to know is that the mesosphere is where most meteors burn up upon entering the atmosphere.

Thermosphere
I understand even less of this stratigraphical layer, for a confusing reason the temperature increases with altitude although not for the same reason as in the stratosphere. It's something to do with there being so few particles, I don't know google it.

Exosphere
There's like nothing here, at all. The number of particles (mainly hydrogen and helium) are so few that they can travel hundreds of kilometres without colliding with each other, this also means that the atmosphere stops behaving like a liquid. "Why are you even telling us this then?" You may be wondering... Well it sort of answers a question raised in class the other day about whether atoms in Space join Earth's atmosphere. It is actually the opposite, Earth experiences a net loss of hydrogen and helium at about 3 kg and 50 g respectively a second. That's a relatively tiny amount though so don't start worrying that we're running out of atmosphere.

The human race will have likely imploded before we ever lose our atmosphere.

Friday, 18 February 2011

Encounters at the End of the World

This is one of the best films I have ever seen and has made me definitely want to visit Antarctica before I either die or it becomes 'westernised'. The view I have of Antarctica is one of never-ending snow and ice with a vast biodiversity under the ice in the ocean. Most of the continent is still like that apart from McMurdo which in the Spring/Summer becomes a normal functioning town with a population of about 1000, that kind of disappointed me but I suppose there needs to be a central hub to act as a base.

What I dislike about McMurdo is easily made up for with its inhabitants. They range from the adventurous to the pure weird. One former philosopher states that he thinks all the people who are a bit strange and like to explore end up in Antarctica, a theory later backed up by a linguist who describes that "all people who aren't tied down fall to the bottom", in this case Antarctica. If you're thinking these people are a bit odd then they're nothing compared to a plumber who believes that he's descended from the Aztec royal family or the Bus driver (former Banker) who once got chased by the Mayans because they thought he was a child catcher. Although strange you get the sense that these people live here because they really love it, the linguist also raises a very thoughtful point. We try to solve all kinds of biodiversity needs/climate change/stop deforestation etc. yet in 2005 it was reported that we were losing a language at the rate of one a fortnight. Should we focus on protecting our cultural heritage as much as the environment?

What I find remarkable about Antarctica is how people describe it as an incredibly peaceful place and the next minute they're dynamiting the ice to create a dive hole. I don't think it's a problem, just a bit strange. The scientist explains that some of the creatures in the deep seem like they're out of a sci-fi film and once the camera descends into the waters it's easy to tell why. In the darkness of the ocean looks mean nothing, it doesn't matter if you have rainbow scales what you actually need are some sharp spines. The ecosystem here is one of the most violent and extraordinary on the planet. The divers are looking for are the most primitive forms of life, trying to understand how life could have formed in the first place. The cameraman captures the moment when they state they've potentially found a new species, something which they claim to be remarkable. The head scientist continues eating his cereal.

One of my favourite moments in the film is when they visit a scientist who has worked in isolation with penguins for so long that he doesn't really enjoy talking to humans anymore. You can tell that Herzog has to try and keep a dying conversation going. The extent can be seen by the fact that Herzog has to ask if there are gay penguins and if they can go insane. It's the most surreal conversation in the film without a doubt.



The film also visits Mt Erebus which allowed me to construct a new view of volcanologists. They're quite strange but then again so is everyone on Antarctica... Volcanologists visit Erebus as it's easier/safer to visit than Congo and Kenya which are the only other places where volcanoes with exposed inner magma are found. As you'd expect the volcanologists are dressed up in thick layers of thermal equipment apart from Professor Clive Oppenheimer from Cambridge who's wearing... tweed.

I can't recommend this film enough. It's unbelievable, I loved it and think I'll probably watch it again at some point. Werner Herzog's gruff German accent is perfect for the documentary which has been filmed so brilliantly. It's definitely up there with my favourite films.

Sunday, 13 February 2011

Week 6 - Nothing?

I apologise for the lack of post this week geographers.
I spent all of Saturday working and then 9 hours today recording an EP with my band, I will however be updating this tomorrow... as long as the field-trip doesn't prevent me.

James