COMPONENTS, ELEMENTS AND CONTROLS OF CLIMATE (Lecture 1)
Spatial variations in climate Climate as a system
Temporal variations in climate (Seasonal) Climate as a system
Temporal variations in climate (Seasonal) Climate as a system
Long-term changes in climate Climate as a system
Components of the Climate System
Radiation Scattering and Albedo
Eccentricity (orbital stretch) Shape of Earths yearly path around sun Earths orbit is not perfectly circular: elliptical shape Orbit shaped by gravitational pull of planets Eccentricity is NOT constant (~100ky & 400ky) Eccentricity is SECONDARY reason for seasons
Eccentricity (orbital stretch) Affects amount of energy reaching Earth!
Obliquity (axial tilt) The tilt of axis of rotation relative to the plane of the Earths orbit about the Sun
Obliquity (axial tilt) Obliquity NOT constant: 22.1°-24.5° variation (~41ky) Affects global distribution of solar energy!
Obliquity (axial tilt) The PRIMARY cause of the seasons
Simple Change in Axial Tilt No tilt, solar radiation always over equator No seasonal change in solar radiation Solstices and equinoxes do not exist 90° tilt, solar radiation hits poles Day-long darkness Day-long light Extreme seasonality
Precession (Earth wobble) Earths spin axis wobbles, gradually leaning in different directions (direction of leaning or tilting changes through time)
Precession (Earth wobble) Caused by gravitational pull of Sun + Moon One circular path takes 25,700 years Earths rotational axis points in different directions through time
Precession (Earth wobble) Earths wobble and rotation of its elliptical orbit produce precession of the solstices and equinoxes One cycles takes 23,000 years
Precession (Earth wobble) Affects climate by changing the global distribution of solar energy Today VS 11,500 yrs ago
OVERALL CLIMATIC EFFECT OF ORBITAL CHANGES
Sunspots and Dustclouds Sunspot:
END LECTURE 1
CONTROLS OF CLIMATE (Lecture 2)
Climate as a System
Pressure DECREASES with height! (Think: swimming pool)
Energy and the Atmosphere Solar Radiation EARTH Atmosphere
Energy and Latitude
Vs.
Perpendicular Surfaces get More…
Energy and Latitude
Daily changes in insolation at the Earths surface The sun does not get bigger/hotter throughout the day… It just changes position!
How does differential heating cause climate zones?
Hadley Cells (super simple version)
Hadley Cells (simple version) What causes multiple cells? Why do winds curve? What do all these have to do with climate and climate zones?
End Lecture 2
CONTROLS OF CLIMATE Part 2 (Lecture 3)
Hadley Cells (super simple version)
Hadley Cells (simple version) What causes multiple cells? Why do winds curve? What do all these have to do with climate and climate zones?
Coriolis Force Effect
Coriolis, winds and cloud patterns
Hadley Cells (simple version)
Convergent/Divergent Zones Convergent Divergent (at Earths surface)
3 Main Pressure Belts Easterlies Westerlies Trade Winds
ITCZ
ITCZ and Equatorial Rainforests
Polar Front
Polar Fronts and Boreal Forests
Subtropical High
Subtropical Highs and Deserts
Polar Highs and Tundra Why isnt it a desert in the N and S poles? 1. Not enough sunlight… 2. Thinner atmosphere
Putting it all together…
Points to Ponder… Why are deserts/forests patchy instead of stripy? Why are some glaciers found in rainforests and some rainforests found in deserts?
End Lecture 3 Next lecture: Regional/Local Controls of Climate
REGIONAL AND LOCAL CONTROLS OF CLIMATE (Lecture 4)
Hadley Cells and Global Climate
0°0°30°60°90° N. Pole 30°60° 90° S. Pole All seasons wet All seasons dry All seasons wet All seasons dry
Non-uniformity of Global Climate Why patchy and not stripy? LISBON, PT OMAHA, NE, USA
Non-uniformity of Global Climate Lisbon, PT: (Latitude 38°N) Avg. Min. Temp. = 8°C (Jan) Avg. Max. Temp. = 28°C (Aug)
Non-uniformity of Global Climate Omaha, NE, USA: (Latitude 41°N) Avg. Min. Temp. = -6°C (Jan) Avg. Max. Temp. = 23°C (Aug)
Water takes longer to heat than land
Water has a moderating effect on land temperature
Water takes longer to cool than land
Water has a moderating effect on land temperature
Water Moves Heat To/From Areas
Thermohaline Circulation 1. Sun heats water around the equator 2. Surface currents take warm water north (N. Atlantic)
Thermohaline Circulation 3. Surface water cools as it heads to high latitudes (heat released to the atmosphere) 4. Cool/salty water sinks and heads south
Thermohaline Circ. is what keeps Western Europe warm! Dublin, IEMinsk, BY
Lyon, FR Lucerne, CH
201 meters436 metersElevation
End Lecture 4 Next lecture: More Regional/Local Controls of Climate
MORE REGIONAL AND LOCAL CONTROLS OF CLIMATE (Lecture 5)
0°0°30°60°90° N. Pole 30°60° 90° S. Pole All seasons wet All seasons dry All seasons wet All seasons dry
3 Main Pressure Belts Easterlies Westerlies Trade Winds
GULF STREAM KEEPS WESTERN EUROPE WARMER THAN IT OUGHT TO BE (CONSIDERING LATITUDE)
Land-Sea Night Temp. Differences
NIGHT TIME THERMAL INFRARED IMAGE SHOWING : WATER WARMER THAN LAND
More Regional/Local Climate Factors
Seattle, WA Yakima, WA
More Regional/Local Climate Factors
The Influence of Topography on Climate 1. Promoting convection Cooler Air Warm Air
2. Forcing air to rise along windward slopes AIR MASS PREVAILING WIND DIRECTION OROGRAPHIC UPLIFT: The vertical forcing of air by terrain features such a hills or mountain The Influence of Topography on Climate
Orographic Uplift and Climate Uplifted air cools and releases moisture contents AIR MASS PREVAILING WIND DIRECTION Precipitation greater if air mass is from a water body
Aspect and Climate Uplifted air (now dry) crosses ridge and descends… Air heats adiabatically Hot, dry air continues onward… 3. Forcing air to sink along leeward slopes
Aspect and Climate Wet, windward aspect VS. Dry, leeward aspect (RAINSHADOW) Rainshadow: An area of diminished precipitation on the lee side of mountains
Karijini National Park, W. Australia
Complex Combinations of Topo + H 2 O…
WINTER Prevailing Winter Winds
LAKE EFFECTS
End Lecture 5 Next lecture: Urban Climates and Mans Effect on Climate
REGIONAL AND LOCAL CONTROLS OF CLIMATE: URBAN CLIMATES (Lecture 6)
Surface Type: Urban Surface and Insolation
Different surfaces have different albedos Different capacities to absorb insolation Surface~Albedo Snow0.98 Grassy field0.20 Farmland0.15 Swampland0.14 Asphalt0.07 Ocean0.03
Surface Type: Urban Surface and Insolation
Surface~Specific Heat (J/kg·K) Water (at 0°C)4218 Wet soil1480 Asphalt920 Concrete880 Brick840 Tin228 Surface Type: Urban Surface and Insolation
Evapotranspiration (ET) = Evaporation (E) + Transpiration (T)
The majority of clouds over rainforests are generated by rainforests Less rainforests less clouds less albedo warmer temperatures
Forward looking infrared (FLIR)
(Relatively) Natural Landscape Urban Landscape
Urban Structures
Day: Insolation channelled and trapped
Night: Thermal energy channelled and trapped
Wind flow hindered Advection diminished
Urban heat islands Most cities show a large heat island effect, registering 5–11°C warmer than surrounding rural areas
Urban heat islands dark surfaces such as asphalt roads or rooftops can reach temperatures 30–40°C higher than surrounding air
End Lecture 6 Next lecture: Urban Pollution and Urban Climate Climate Classification (bring pillows)
Urban Climate (Pollution) & Climate Classification Systems
Urban Heat Island
Surface Type and Radiation Balance
Effect of Atmosphere on Radiation Balance
Particulate matter in the atmosphere tend to reflect insolation Cools the Earths surface
Effect of Atmosphere on Radiation Balance Particulate matter in the atmosphere tend to absorb and re-radiate thermal energy Warms the Earths surface
How Greenhouses Work Result: Interior of greenhouse warms 1. Glass walls/ceilings allow short-wave radiation (i.e. light) into greenhouse (1) 2. Radiation absorbed by ground/objects in the greenhouse, which then re- radiate it as long-wave radiation (i.e. heat) (2) 3. Glass walls/ceilings prevent long-wave radiation from leaving (3)
How greenhouse gases work
Effect of Atmosphere on Radiation Balance Human activity adds more particulate matter and GHGs into the atmosphere Air pollution affects climate globally and causes other environmental damage (e.g. acid rain, water pollution, etc.)
Urban climates are especially affected because air pollution concentrated over urban landscape Effect of Atmosphere on Radiation Balance Bogotá, CO Los Angeles, US
Effect of Atmosphere on Radiation Balance GHGs/Particulate Matter Urban-generated heat Heat absorbed and re-radiated
Climate Classification Systems
Climate/weather stations in IE
End Lecture 7 Next lecture: More Climate Classification
More Climate Classification Systems
Group A
Group B Desert Steppe
Group C Med. Humid Sub-Trop Maritime Temperate Maritime Sub-Arctic
Group D Opposite Extreme Temperatures Throughout Year
Group E Et Ef
Major Climate Groups (Koppen System)
End Lecture 8 Next lecture: Finish Climate Systems… Monsoons
K ö ppen System & Monsoon Climate
Major Climate Groups (Koppen System)
Monsoon Climate
Water takes longer to heat than land Sea Breeze
Water takes longer to cool than land Land Breeze
Asian Monsoon
When would be the best time to climb Mt. Everest: Winter or Summer?
North American Monsoon
African Monsoon Two peaks: 1)Late spring (May/Jun) 2)Late summer (Jul/Aug)
End Lecture 9 Next lecture: Climate & Human Physiology
Climate & Human Physiology Comfort and Clothing
Climate and Physiology
Wind Chill Wind chill (not wind chill factor): The apparent temperature felt on exposed skin due to the combination of air temp and wind speed
Effects of Humidity Heat Index (HI): index that combines actual air temperature and relative humidity to determine an apparent temperature
End Lecture 10 Next lecture: Clothing and Survival in Extreme Climates Climate & Agriculture/Horticulture
Climate & Human Physiology Comfort and Clothing
Clothes can impact your survival in extreme climates
Clothing and Survival in Extreme Climates Heat gain in desert: 1. Direct insolation 2. Reflected insolation 3. Conductive heat gain 4. Advective/Convective heat gain
Clothes can impact your survival in extreme climates
Clothing and Survival in Extreme Climates
Clothes can impact your survival in extreme climates
Climate & Agriculture
End Lecture 11 Next lecture: Climate & Agriculture/Horticulture
Climate & Horticulture
Wind Wind-sensitive crops (e.g. vines/grapes) ideally situated in relatively wind- calm areas Ex: S. Australia Central California S. France If located in wind-prone areas, climate must be modified (e.g. the use of windbreaks)
End Lecture 12