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what is a diurnal energy budget?
the diurnal energy budget refers to the balance between incoming and outgoing energy over a 24-hour period (one day and night cycle)
what does the diurnal energy budget help explain?
it helps explain:
daily temp changes
how energy is distributed during the day and night
what are the 6 factors affecting the diurnal energy budget?
1) incoming solar radiation (insolation)
2) reflected solar radiation (albedo effect)
3) surface and sub-surface absorption
4) sensible heat transfer
5) latent heat transfer
6) longwave radiation
how does insolation (incoming solar radiation) work?
the sun emits shortwave radiation
some is absorbed by the Earths surface warming it
some is reflected back by clouds, water, and ice (albedo effect)
what are some factors affecting the amount of insolation received?
time of day
latitude
season
cloud cover
how does reflected solar radiation (Albedo effect) work?
some of the incoming solar radiation is reflected back into space?
albedo is a measure of how much radiation is reflected by a surface
Light coloured surfaces (fresh snow, ice, and sand) have a high albedo (reflect more)
Dark Coloured surface (forests, oceans, asphalt) have a low albedo (absorb more)
what are some factors affecting albedo?
Thick clouds reflect more sunlight (cooling effect)
thin clouds trap heat at night (warming effect)
how does surface and sub-surface absorption work?
some solar energy is absorbed by land, water and vegetation
land heats quickly, water heats slowly
darker denser materials absorb more heat
this stored energy is later released as heat
how does sensible heat transfer work?
heat change that is felt - heat is transferred between the surface and air via..
Conduction:
direct heat transfer between the ground and air
Convection:
warm air rises, cool air sinks, creating air movement (winds)
winds help redistribute heat, cooling some areas and warming others
how does latent heat transfer work? (evaporation)
heat change is not felt - but is when water changes state
evaporation: when water evaporates it absorbs heat (Cooling effect)
evaporation occurs when water absorbs heat and turns into vapour, cooling the surface.
this happens more in oceans, lakes, and humid areas
wind increase evaporation, removing heat faster
how does latent heat transfer work? (condensation)
when water condenses and forms clouds it releases heat
releases heat into the air - slows down heat loss at night
condensation happens when air cools, causing water vapour to form dew
this releases latent heat into the atmosphere, slightly warming the air
how does latent heat transfer work on clear nights? (condensation)
on clear nights with no clouds to trap heat, temps drop quickly. but if condensation occurs, some heat is released, preventing extreme cooling
how does longwave radiation work?
the earth emits heat as long wave radiation (usually at night)
some of this escapes into space, while some is trapped by greenhouse gases.
Clear nights lose more heat, making them colder
which of the 6 factors affecting the diurnal energy budget occur in the day, night or both?
Day:
incoming solar radiation
reflected solar radiation (albedo)
surface absorption
Night:
Longwave Radiation
Day and Night:
sensible heat transfer
latent heat transfer - evap: day, condensation: night
what is the global energy budget?
the global energy budget is the balance of how much energy is received from the sun amd how much energy is radiated back to space
what does the global energy budget’s balance control?
it controls the earth climate and temperatures
what are the 4 differences between the global energy budget and the diurnal energy budget?
Timescale
scope (boundary range)
main factors
processes
what is the difference in the GEB and DEB in terms of timescale?
Global:
Long-term (measured over years or decades)
Diurnal:
short-term (daily cycle)
what is the difference in the GEB and DEB in terms of scope?
GEB:
entire earths energy balance
DEB:
energy balance at a specific location over a 24-hour period
what is the difference in the GEB and DEB in terms of their main factors?
GEB:
insolation, albedo, greenhouse effect, outgoing radiation
DEB:
day time heating and nighttime cooling, cloud cover, surface type
what is the difference in the GEB and DEB in terms of processes?
GEB:
includes large-scale climate influences like GHG’s and long-term climate change
DEB:
focuses on local effects like morning warming, peak afternoon temps, and night cooling
what is the Greenhouse effect and why is it so important?
It traps in the Earth’s atmosphere warming the surface and keeping it stable at and average of 15 degree’s. Without it, earths avg temp would be -18 degrees (very cold!)
what do greenhouse gases do?
absorb and re-radiate heat back to Earth
what are the 4 major GHG’s and what do they come from?
Carbon Dioxide - from burning fossil fuels, deforestation
Methane - from livestock, rice farming, and landfills
Water Vapour - natural but increases with warming
Nitrous Oxide - from agriculture, fertilizers
what is the enhanced Greenhouse effect?
caused by human activities - burning fossil fuels, farming etc) increase the concentration of GHG’s
more heat is trapped rather than radiated out to space - warming the earth
this leads to global warming and climate change
Projected warming:
1.5 degrees by 2050
2-4 degrees by 2100
what are the 3 factors affecting the Global Energy Budget?
Latitude (excesses and deficits)
atmospheric transfers: (wind belts and ocean currents)
seasonality
what is latitude?
latitude is the measurement of a locations distance, north or south of the equator
expressed in degrees
the equator is 0 degrees latitude
the north pole is 90 degrees North
the south pole 90 degrees South
what is the importance of latitude in terms of energy balance?
areas near the equator receive more direct insolation while high latitudes receive less due to the angle of sunlight
what is the importance of latitude in terms of climate patterns?
different latitude zones have distinct climates (e.g tropical, temperate and polar)
what is the importance of latitude in terms of seasons and daylight?
higher latitudes experience more variation in daylight hours throughout the year
what are the three main ways that latitude impacts the global energy budget?
1) unequal solar energy distribution
2) excess (surplus) and deficit zones
3) heat redistribution
explain how latitude impact the GEB by its unequal solar energy distribution
the earth is curved, so different latitudes receive different amounts of solar energy
Low Latitudes get more direct sunlight = high angle of sunstrike = high insolation = energy surplus
High Latitudes get more spread out sunlight = low angle of sunstrike = spreads energy over a larger surface area = deficit
finish the sentence..
“the equator receives about……as much solar energy per unit area as ……….”
“the equator receives about twice as much solar energy per unit area as the poles
what is the tilt of the earth?
23.5 degrees
what is the latitude or areas where there is an energy surplus
Energy Surplus: (Between 350N and 350S)
what is the latitude or areas where there is an energy deficit
Energy Deficit: (Above 350N and Below 350S)
what do high latitudes rely on heat transport from (Between 350N and 350S)
from lower latitudes through winds and ocean currents
what does the latitudes (Between 350N and 350S) drive?
the Hadley cell circulation which redistributes heat
what redistributes heat energy from the equator?
Winds and ocean currents
what do cells in atmospheric circulation do?
Hadley, Ferrel and Polar cells move warm air poleward and cold air equatorward
what do ocean currents do (warm and cold)?
warm currents (Gulf Stream) transfer heat from the tropics to higher latitudes
while cold currents (Peru Current) bring cold water toward the equator
what is a perfect sentence to explain how latitude affects the global energy budget?
Latitude controls the distribution of solar energy, creating a global pattern of energy surpluses at low latitudes and energy deficits at high latitudes. This imbalance drives global atmospheric and oceanic circulation. helping to regulate Earth’s climate
what are the differences between warm and cold air?
warm air expands - cold air contracts
warm air is less dense - cold air is denser
the warm air rises - the cold air sinks
warmer places have low air pressure - colder places have high air pressure
what are the three cells that make up the tri-cellular model
Hadley cell
Ferrel cell
Polar cell
what latitude is the Hadley cell and what circulation is it?
the latitude is (0o - 30o)
and its a tropical circulation
what is the largest and powerful cell
the Hadley cell
How does the Hadley cell work?
1) intense solar heating at the equator causes air to rise
2) the rising air cools and condenses forming clouds and heavy rain
3) the air moves toward the poles at high latitudes and sinks at 30o
4) the sinking air moves back toward the equator as the “Trade Winds”
what latitude is the Ferrel cell and what circulation is it?
the latitude is (30o - 60o)
Mid-Latitude Circulation
what is the Ferrel cell and what is it driven by?
The Ferrel Cell is an indirect cell, driven by the Hadley and Polar cells
how does the Ferrel cell work?
1) Air at 30o latitude sinks (from the hadley cell) creating the high pressure
2) some of this air moves toward the poles rising again at 60o latitude
3) This rising air fuels storm systems and wet climates at mid-latitudes
what winds does the Ferrel cell drive?
The Ferrel cell drives the Westerlies (West to East)
what latitude is the Polar cell and what circulation is it?
the latitude is (60o - 90o)
Cold Air circulation
what is the smallest and weakest of all the cells?
Polar cell
how does the polar cell work?
1) cold dense air sinks at the poles
2) this air moves toward 60o latitude, where it meets the warm air from the ferrel cell
3) the warm air rises, creating low pressure and stormy conditions
what are wind belts?
large scale patterns of wind circulation caused by the Earths rotation and uneven heating.
what is the coriolis effect?
caused by the Earths rotation it deflects winds to the right in the Northern hemisphere and to the left in the southern hemisphere
how are winds formed?
1) unequal heating of the Earth’s surface
warm air rises, creating a low-pressure area
cool air sinks, creating a high pressure area
2)) air moves from high to low pressure - needs to balance
air moves horizontally from high pressure areas to low-pressure areas: this movement is wind
3) The coriolis effect changes wind direction
because the earth rotates, moving air does not travel in a straight line
so the CE deflects wind
4) near the ground obstacles like mountains forest etc slow down windspeed and change its direction slightly.
higher in the atm, winds are faster because there is less friction
what are the 4 main winds
Trade Winds
Westerlies
Polar Easterlies
Jet Streams
what is an ocean current?
a continuous of seawater in a specific direction, typically caused by factors like wind, temperature differences, salinity, and the Earths rotation
how does the land and sea absorb heat differently
oceans heat up 5 times slower than land
oceans have a higher heat capacity
oceans absorb more radiation from the sun
oceans lose more heat slowly
what do warm surface currents do?
they move warm water from the equator towards the poles by convection
as they flow, they transfer heat to the atm warming nearby costal regions
what is an example of a warm ocean current?
The Gulf stream in the Atlantic
keeps Europe milder in the winter compared to N. America on the same latitude
where is the gulf stream?
North Atlantic Ocean - orginates in the Gulf of Meixco and flows along the eastern coast of NA into NW Europe
what does the Gulf Stream do and what is it caused by?
redistributes heat and influences climate patterns on both sides of the Atlantic
its caused by the earths rotation and the Westerlies
the Gulf Stream has an impact on three continents what are they?
North America
Europe
Africa
what is the impact of the Gulf Stream on North America’s climate
warm air and moisture, increasing humidity
hurricanes along the East Coast
Keeps winters along the SE US milder compared to inland areas
what is the impact of the Gulf Stream on Europe’s climate
warm waters to northwestern Europe, moderating winter temps
without it, Europe would have a much colder climate, similar to parts of Canada at the same latitude
what is the impact of the Gulf Stream on Africa’s climate
influences West African monsoons, affecting rainfall patterns
what do cold ocean currents do?
they move cold water from polar regions toward the tropics (convection)
these currents help cool the air above them, influencing local climates and reducing evaporation rates
what is an example of a Cold Ocean current
the Humboldt Current
where is the Humboldt current located?
South Pacific Ocean
flows Northwards from Chile, along the west coast of South America towards Peru
what is the purpose of the Humboldt current
it redistributes heat globally, but also allows nutrient rich water to rise to the surface, supporting large ecosystems
what is the Humboldt current caused by?
Southeast trade winds pushing surface water westward, allowing cold water to rise
what are the impacts of the Humboldt on climate?
the cold water lowers temps along the west coast of America making it cooler and drier than other costal areas at the same latitude
it reduces rainfall by preventing warm air from rising contributing to desert conditions
what are the impacts of the Humboldt on climate, in terms of El Nino?
the Humboldt current affects global climate through its role in El Nino and La Nina events
what does el nino do?
it weakens the humboldt current, causing warmer water, heavy rainfall and droughts
what does la nina do?
la nina strengthens the current, bringing cooler temps and drier conditions
what is the thermohaline circulation (conveyor belt)
this moves warm and cold water between the surface and deep ocean layers
what is the process of thermohaline circulation (conveyor belt)
warm water from surface currents cools as it moves poleward - becomes denser and skinks forming deep cold currents
these cold currents slowly circulate back toward the equator
rising again through upwelling, completing the cycle
what is ocean upwelling?
a process where cold, deep, nutrient-rich water rises to the surface to replace warm surface water that has been pushed away.
what is the process of ocean upwelling?
1) wind driven movement
upwelling occurs when strong winds blow surface water away from a coastline or the open ocean
2) replacement by deep water
as surface water moves, cold, nutrient rich- water from deeper layers rises to replace it
3) Nutrient boost
this deep water is rich in nutrients like nitrates and phosphrates, which fuel plankton growth, supporting rich marine ecosystems
what effect does ocean upwelling have?
a cooling effect: upwelling brings cooler water to the surface, lowering regional sea surface temps and influencing atmospheric circulation
what is ocean upwellings impact on climates?
upwelling regions experience:
cooler sea surface temps leading to drier conditions because of reduced eaporation
what is seasonality?
seasonality is the yearly change in weather, temperature and daylight. It happens because the Earth tilts at a 23.5-degree angle as it moves around the sun.
when does summer occur
when a hemisphere is tilted toward the sun
when does winter occur
when a hemisphere is tilted away from the sun
are days longer in summer or winter
summer
when is summer and winter in the southern hemisphere
Summer:
December to February
winter:
June to August
when is summer and winter in the northern hemisphere
Summer
June to August
Winter
December to February
what does the ITCZ stand for
intertropical convergence zone
what happens with the ITCZ and wind belts during seasons
they shift north in July and South in Decmber
this brings intense solar heating to their areas
what are monsoons?
seasonal wind patterns that result from the differential heating of the land and sea
what is the case study for monsoons
The indian Summer Monsoon
what are the causes of the Indian summer monsoons
april - may: intense heating of the Thar Desert (40 - 50 degrees) due to differential heating and latitude
The ITCZ moves northwards: this strengthens the winds blowing in and brings heavy rains due to the low pressure belt acompanying it