Water Cycle - Weather (5)
Pre Lab 

   
OBJECTIVES:
  • Exploring the relationship of land and water.
  • Interpreting data from the Pacific Ocean.
VOCABULARY:
  • climate
  • continental
  • marine
MATERIALS:
  • crayons
  • inflatable world globe
  • Internet
  • worksheet

Students compare ocean and land climates.

BACKGROUND:

The land is usually divided into climatic zones which refer to the general overall weather in the region. These climate zones also take into consideration precipitation, temperature, type of vegetation it can support, and other factors. On the figure included in this lesson, the following divisions can be defined: 

  1. Tundra (cold, with little vegetation, high precipitation)
  2. Boreal forest (cold, forest, high precipitation)
  3. Temperate (moderate temperature)
  4. Desert (dry climate, little vegetation)
  5. Savannah (moderate precipitation, grassland)
  6. Steppe (cool climate; little vegetation)
  7. Tropical Rain Forest (warm, high precipitation, forest)
  8. Ice caps (cold, snow, no vegetation).

On the ocean there are also east-west trending zones which can be divided into polar, subpolar, temperate, subtropical, trades, equatorial, and monsoons. These surface waters affect the local climate, especially in the intensity and duration of wind. When there are unusual warm or cold waters in the ocean, they cause the air masses to move in different direction which can change the weather patterns severely. El Nino, a periodic condition of a warming of the waters in the Pacific is one of these phenomena.

In polar ocean area ice occurs at the surface most of the year and surface temperatures are at or near the freezing point. In winter there is little direct sunlight. In subpolar regions sea ice is seasonal, and may disappear in the summer. Surface water temperatures may rise to 5ºC. The temperate regions correspond to westerly winds where there are severe storms. Heavy precipitation and strong seas are present. In subtropical regions the winds are weak and surface currents are not strong. Clear skies, dry air, and abundant sunshine creates a high evaporation rate. In equatorial regions surface waters are warm with warm, moist air that produces high precipitation.

PROCEDURE:
  1. Go over the background information with students. The inflatable world globe with biomes on it also defines the different climatic zones. Students should look at the globe to find the limits of each region that you discussed.
      
  2. With the information have them design a way to show this information on the worksheet. You may want to give them clues, that color coding the information will help make a reader see areas that are warm versus cool easy. Basically, students make a color coded legend and color the appropriate region.
      

  3. Climate Diagnostic Center of the National Oceanographic and Atmospheric Agency. You may want to see if this years climate actually coincides with this generalized pattern

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