chapter 2 Flashcards
Why does the earth have seasons?
Due to the tilt of the earth’s axis. As the Earth revolves around the sun, this tilt means that different parts of the planet receive more direct sunlight at different times of the year, creating seasons
Explain why the Northern and Southern Hemispheres do not experience the same seasons at the same time.
Because when the Northern hemisphere is tilted towards the sun, the South hemisphere is tilted away from it and vice versa.
Explain why the equator generally has warmer temperatures than the poles.
Because the earth is a sphere, the sunlight hitting the equator is much more intense
Explain differences in length of day at different latitudes at different times of year. (Ex: Today, Bellevue will have 9 hours, 39 min of sunlight, but Phoenix, Arizona will have 10 hours, 40 min. of sunlight. Why is this so?)
Additionally, the days become a little longer at the higher latitudes (those at a distance from the equator) because it takes the sun longer to rise and set.
Explain why the amount of daylight changes throughout the year (shorter days in winter, longer in summer).
As the tilt of the earth towards the sun, the amount of sunlight received at a given point changes
- Explain how and why the path of the Sun changes in the sky from one season to the next.
During summer in the northern hemisphere, the Sun rises north of east and sets north of west. It is high in the sky at noon. During winter in the northern hemisphere, sunrise and sunset appear farther south along the horizon.
Differences between weather and climate
Weather is short term, climate is more long term trends
How the tilt of the earth impacts climate on earth
Impacts seasons, causes more extreme seasonal variation closer to the poles
How wind patterns and the atmosphere influence climate
Redistribute heat and water
How ocean currents impact climate
Transporting warm water and precipitation from the equator toward the poles and cold water from the poles back to the tropics.
How does topography impact climate
Bodies of water – milder climates, absorb solar radiation and very slowly emit it
Mountainous – more extreme weather, block movement of air and moisture
Coriolis Effect and how it affects the movement of air currents on Earth
air moving in a straight path appears to curve to the right in the Northern Hemisphere and to the left in the Southern Hemisphere due to the earth’s rotation. causes large scale wind patterns that impact the formation of hurricanes
Convection currents in air (atmosphere) and water (oceans), considering changes in temperature, density, and pressure
Warmer, less dense air/water rises, and cooler, more dense air/water sinks, causing circular patterns.
In the air: cause large scale wind patterns (e.g. hadley cells, polar cells) and impact climate. There is a pressure diff between high pressure cold air and low pressure hot air zones, the stronger the pressure diff the stronger the winds
In the water: create cold currents in the deep ocean and warm surface currents
Hadley cells
Convection currents
Located between equator and 30 degree latitude
Hot air rises after gaining lots of heat from solar radiation, creating a low pressure zone at the equator. This air travels towards the poles and cools and sinks at lat. 30 degrees, creating low pressure zones.
This creates trade winds and contributes to the formation of rainforests at the equator
Ferrel cells
Mid-latitude atmospheric circulation cell (30-60) where air near the Earth’s surface flows poleward and eastward, while at higher altitudes it moves equatorward and westward. opposite of hadley cells.
responsible for the prevailing westerly winds in those regions.
unstable weather conditions like mid-latitude cyclones and fronts due to the mixing of warm and cold air masses.