defining climate
DESCRIPTION
Defining Climate. Ch. 14. 1. Climatology. Climatology : the study of Earth’s climate and factors that affect past, present, & future climate changes. Climate : long-term weather patterns of an area. Includes annual (yearly) variations of temp, precip , wind, & other weather variables. - PowerPoint PPT PresentationTRANSCRIPT
Defining Climate
Ch. 14. 1
Climatology• Climatology: the study of Earth’s
climate and factors that affect past, present, & future climate changes.• Climate: long-term weather patterns
of an area.–Includes annual (yearly) variations of
temp, precip, wind, & other weather variables.
Climatology• Normals: data averaged monthly or
annually for 30 years & become the standard values for a location.–Data includes: high & low temp, amt.
of rainfall, wind speed & direction, humidity, & air pressure.–Not intended to describe usual
weather conditions.
Causes of Climate• Climatic differences caused by…–Differences in latitude–Topography–Closeness of lakes & oceans–Availability of moisture–Global wind patterns–Ocean currents–Air masses
Differences in Latitude• Different areas of Earth received different
amounts of solar radiation because of the tilt of Earth when facing the Sun.– Creates climate zones found in each hemisphere.
Latitude & Climate Zones• Tropics– Found between 23.5 North and South and the equator.– Warm nearly year-round.
• Temperate Zones– Found between 23.5 and 66.5 degrees North and
South of the equator.– Temperatures are moderate (warm and cold).
• Polar Zones– Found between 66.5 North & South of equator to the
poles.– Temperatures tend to be very cold.
Climate Zones
Topographical Effects• Large bodies of water affect climate.–Water heats up and cools down slower
than land.–Many coastal regions are warmer in
winter & cooler in summer than inland areas at similar latitudes.
• Temp decreases in areas of HIGHER altitude.–Mtns are colder than sea level areas.
Topographical Effects• Climates differ on either side of mtns.–Windward side: side of mtn where air
rises and condenses to form clouds and drops moisture = wet & cool.–Leeward side: opposite side of
windward side, air is drier & warmer as it descends = deserts are common here.
Topographical Effects: Orographic Lifting
Air Masses• Recall #1: Air masses have distinct
regions of origin, caused by differences in amount of solar radiation.• Recall #2: Properties also depend on if
they are formed over water or land.• Air masses will reflect the
characteristics of that areas climate.
Air Masses