U2L3 Oceans and Climate Flashcards
What is a similar pattern corresponding to settlements?
A similar pattern is seen in other cities: as settlements move inland, expect higher summer highs, lower winter lows, and greater daily variation in the temperature.
Example:
The pattern is even seen near the Great Lakes. Milwaukee, on the shores of Lake Michigan, has milder summers and winters and smaller daily swings in temperature than Madison, 129 k (80 mi.) inland.
How can a body of water change the temperature?
A large body of water will soak up heat when it is warm and release it when it is cool. This modulating effect on local climate is seen over cycles of both the day and the year. On a longer and planet-wide scale, Earth’s oceans regulate the temperature of the planet as a whole. The oceans absorb much of the incident solar energy and later radiate that energy back into the atmosphere.
The light that reaches the Earth’s surface is what type of wavelength?
The light that reaches Earth’s surface is largely in the visible and near infrared range of wavelengths.
What is definition of near infrared?
Wavelengths of electromagnetic energy just outside the visible light wavelengths
How are the way sunlight interacts with landmasses and sunlight different?
Unlike landmasses, where solar energy is absorbed in a thin layer at the surface, sunlight can penetrate seawater to a depth of tens of meters. In addition to providing a far greater depth over which energy can be absorbed, oceans cover around 70 percent of Earth’s surface—more than twice the area covered by land. Water’s specific heat capacity is about four times that of land, so a section of water can absorb far more energy than an equal area of land before its temperature significantly rises.
True or False.
Most thermal energy at Earth’s surface is stored in the oceans.
True
What is water’s heat capacity compared to land’s heat capacity?
Water’s specific heat capacity is about four times that of land, so a section of water can absorb far more energy than an equal area of land before its temperature significantly rises.
Incident solar energy is strongest where on earth?
At the equator, where the sun’s rays are almost perpendicular to the surface
Most solar energy flows into Earth’s surface near the ____.
Equator
Because solar energy flows mostly near the equator, that is mostly water, what is it’s albedo?
Most solar energy therefore flows into Earth’s surface near the equator, and this region is mostly covered in water, which has a low albedo and is excellent at absorbing thermal energy. Some of this energy returns to the atmosphere through evaporation. It can also be transferred through conduction and convection when a warm ocean heats the cooler air above it.
What is the definition of albedo?
The paleness of a surface
All object with a temperature above absolute zero radiate ____.
Electromagnetic energy
Just a fun little extra info to make you smarter :D
In the tropics, more electromagnetic energy is absorbed than emitted. In the polar regions, more electromagnetic energy is emitted than absorbed. The pattern is energy in at the equator and out at the poles. In the atmosphere, this energy is transferred by wind as warm air rises and cool air sinks. In the ocean, the thermal energy is transferred in ocean currents. Warm water is carried in surface currents toward the poles, where it cools and sinks.
On a sheet of lined notebook paper, draw a circle several inches across. The circle represents Earth, and the spaces between adjacent lines represent equal amounts of incoming sunlight. Near the middle of your circle, which represents areas near the equator, the sunlight is concentrated on a small area. As you move away from the poles the amount of sunlight stays the same, but the area over which it spreads grows larger with latitude. The incoming sunlight per unit of surface area is much greater in the tropics than near the poles.
What are the 3 layers of the ocean?
- Surface waters
- Thermocline
- Deep ocean
Describe the surface water layer of the ocean.
Outside of the polar regions, sunlight provides a lot of thermal energy to this layer of water. Sea surface temperatures are just below freezing at the poles and around 29°C (85°F) at the equator. The surface layer is stirred by wind-driven waves and by tides. When the atmosphere is warmer than the surface water, heat is transferred to the ocean by conduction from the atmosphere, and vice versa when the atmosphere is cooler than the surface water.