nj405.blogspot.com
Geo Blog.: July 2009
http://nj405.blogspot.com/2009_07_01_archive.html
1/5 Aaron. 8/5 Keewei and Chang Jie. 15/5 Farouq and Soma. 22/5 Dat and Chee Chung. 29/5 Manish and XiangKang. Thursday, July 9, 2009. In the following lessons, we had learnt how season and whether contributes. In those lessons, the most complicated is the formation of desert. The location the desert is so unique. After that, we began to explore a new world, which was RIVER. Therefore, I think, to get a better life, we need people to study physical geography. Subscribe to: Posts (Atom).
nj406.blogspot.com
the awesome JH406 is2104 blog.: Rapids
http://nj406.blogspot.com/2009/06/rapids.html
The awesome JH406 is2104 blog. That's right, AWESOME. Monday, June 8, 2009. Subscribe to: Post Comments (Atom). We ♥ geog! 22 extremely awesome people. That's right, AWESOME. You have NO idea (:. As strong as Huiying,. As horny as Jiamin,. As violent as Jiayi,. As shrill as Grace,. As innocent as Valerie,. As despo as Luke,. As inquisitive as Cao Li,. As vertically inclined as Sean,. As dizzy as Zhuhe,. As sleepy as Tri,. As joking as Marcus,. As cheeky as Frank,. As mugger as Joshua,. As lame as Ervin,.
nj406.blogspot.com
the awesome JH406 is2104 blog.: January 2009
http://nj406.blogspot.com/2009_01_01_archive.html
The awesome JH406 is2104 blog. That's right, AWESOME. Monday, January 26, 2009. Composition and Structure of the atmosphere. Troposphere: Up to 15km, which has the highest concentration of gases and also this is where we live. Mesosphere: up to 95/120km, this is where most meteors burn up when it goes to the atmosphere. Stratosphere: up to 50/60km, contains ozone layer. Thermosphere: up to 600km,extremely low pressure, temperature increase with height. Compositions of the earth’s atmosphere:. Is increasi...
nj406.blogspot.com
the awesome JH406 is2104 blog.: Hydrographs
http://nj406.blogspot.com/2009/06/hydrographs.html
The awesome JH406 is2104 blog. That's right, AWESOME. Friday, June 5, 2009. Ok, firstly, hydrographs are graphs which show river discharge over a given period of time. And show the response. Of a drainage basin and its river to a period of rainfall. The discharge of the river is calculated in cumecs/cm 3. Secondly, 2 most important things we must take note of a hydrograph are the lag time. Lag time is the time between the peak rainfall to peak discharge, as stated in the diagram above. In urbanised areas...
nj406.blogspot.com
the awesome JH406 is2104 blog.: Shapes Of Valleys Formed At Various River Courses
http://nj406.blogspot.com/2009/06/shapes-of-valleys-formed-at-various.html
The awesome JH406 is2104 blog. That's right, AWESOME. Wednesday, June 3, 2009. Shapes Of Valleys Formed At Various River Courses. This blog entry is to basically help you understand more about the shape of the valleys formed at the upper course, the middle course and the lower course. Definitions of some of the key words used above:. Erosion: The group of natural processes, including weathering, dissolution, abrasion, corrosion, and transportation, by which material is worn away from the earth's surface.
nj402-geog.blogspot.com
JH402 GEOGRAPHY BLOG! (:
http://nj402-geog.blogspot.com/2009/05/river-features-waterfalls-meanders-and.html
Tuesday, May 5, 2009. River features: Waterfalls, meanders and braidings. This post is about the content of two lessons which are on 28th of April and 29th of April. From: http:/ i1.treknature.com/photos/413/marokopa falls2.jpg). Definition: A waterfall is a sudden step in a river's long profile. From: http:/ www.dkimages.com/discover/DKIMAGES/Discover/previews/774/206846.JPG). Will occur because of the differences in velocity of river flow. From: http:/ 1.bp.blogspot.com/ HTS0iL2pEqg/SX9B79o...From: htt...
nj406.blogspot.com
the awesome JH406 is2104 blog.: February 2009
http://nj406.blogspot.com/2009_02_01_archive.html
The awesome JH406 is2104 blog. That's right, AWESOME. Thursday, February 26, 2009. Today, we discuss about the formation of rain and the distinct kinds of rain. How the rain is formed? There are a lot of causes of the rain such as mountains, low-pressure areas, cold &warm fronts. On this lesson, Miss Lin introduced the rain formed in mountains—the orographic rainfall. The orographic rainfall contains two kinds which are forced uplift and free uplift. OK That is all for today! O(∩ ∩)O. Done by Chen Zhuhe!
nj402-geog.blogspot.com
JH402 GEOGRAPHY BLOG! (:
http://nj402-geog.blogspot.com/2009/04/1st-april-2009.html
Monday, April 6, 2009. Happy April Fool's Day! Sorry for the belated post for the 1st of April Geography Lesson with Mr. Faizal. Anyway, here it is:. We started of on the revision of water balance, where Input = Output. Input consists of the precipitation. And the Output consists of total streamflow (Q), evapotranspiration (E) and storage (S). We then moved on to the section on Hydrographs. Basically, a hydrograph shows how a river reacts to rainfall. So there are 5 main sectors of the Hydrograph. We the...
nj406.blogspot.com
the awesome JH406 is2104 blog.: April 2009
http://nj406.blogspot.com/2009_04_01_archive.html
The awesome JH406 is2104 blog. That's right, AWESOME. Saturday, April 18, 2009. Yesterday, Miss Tang introduced the river system to us! She started off by showing us a picture of the part of the Nile that ran through Egypt. As we observed the picture, we noticed that the Nile looked GREEN. Further up the Nile, away from the delta, there were buildings and much infrastructure as well as some agriculture. Miss Tang then discussed some questions with us. Why are waterfalls and rapids near the source? Howeve...
atmopowerhydroforce.blogspot.com
Super AtmoPower HydroForce Team Go!: Concept Solutions
http://atmopowerhydroforce.blogspot.com/2009/02/concept-solutions.html
Super AtmoPower HydroForce Team Go! Saturday, February 7, 2009. One of the things I get asked quite often is whether or not the solution must be in existence. Well, the answer is both a yes and no. There is no need to reinvent the wheel. If there is a good solution that is already out there that we should push for, why not? On the other hand, if you find that none of the solutions you've found meet the requirements, why not think of one of your own. Here is where it becomes tricky.
