final exam Flashcards

(102 cards)

1
Q

clouds

A

a large aggregation of tiny moisture droplets and ice crystals suspended in air

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2
Q

cloud formation

A

warm air parcel rises and cools
once air parcel reaches dew point temp, it becomes saturated
condensation occurs around a cloud condensation nuclei
a cloud cannot form without this nuclei
a particle >10^-4mm around which condensation occurs and cloud formation begins

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3
Q

natural sources

A

meteoric dust, clay, silt, volcanic material and sea salt

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4
Q

anthropogenic sources

A

sulfur and nitrogen compounds from combustion

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5
Q

cloud forming processes

A

1.collision- coalescence
-temp in the cloud are above freezing (0 deg. C)
-water is in liquid and vapour form
heavier moisture droplets begin to fall & collide with other droplets
-the colliding droplets merge together to form large drops–> rain
2. Bergeron Ice-crystal process
-temps are below freezing
-water is in super-cooled liquid, vapour &ice forms
-air surrounding ice has lower vapour pressure than air surrounding water
-water vapour travels from high to low pressure areas (towards ice)
-water vapour freezes and ice crystal grows (accretion/riming)

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6
Q

cloud classification low: up to 2000m

A
  • Stratus: uniform, featureless grey clouds (stratiform)
  • Nimbostratus: grey, dark, low clouds with drizzling rain (stratiform)
  • Cumulus: grow vertically, can extend into middle level, puffy, billowy flat based clouds with swelling tops, associated with fair weather (cumuliform)
  • Stratocumulus: soft, grey, globular cloud masses in groups or waves (both stratiform & cumuliform)
  • Cumulonimbus: dense, heavy, massive, grow vertically into higher levels, associated with thunder storms, forms anvil shape (cumuliform)
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7
Q

cloud classification middle: 2000m-6000m

A
  • Altostratus: thin to think grey clouds, similar to stratus (stratiform)
  • Altocumulus: globular clouds in groups or lines (cumuliform)
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8
Q

cloud classification high: 6000m-13000m

A
  • Cirrus: wispy, feathery, thin, “mares’ tales” can indicated oncoming storms
    Cirrostratus: (stratiform)
    1. Stratiform: flat, ;layered, with horizontal development
    2. Cumuliform: puffy, globular, with vertical development
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9
Q

Snow

A

precipitation falls through cold layer from cloud to ground as frozen

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10
Q

sleet

A

precipitation falls frozen though cold layer (partially) melts through warm layer
refreezes through cold layer and falls to surface as frozen precipitation
T<0 degree refreeze partially melted
T< -6 degree from >750 m, ice pellets from liquid

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11
Q

freezing rain

A

precipitation falls frozen through cold layer
T<10 deg
melts through warm layer
T>3 deg
rain falls to surface and freezes at surface

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12
Q

Rain

A

falls through frozen cold layer
melts through warm layer
precipitation falls to surface as rain

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13
Q

Hail

A

Originates in a cumulonimbus clouds
raindrops circulate between above and below freezing
Ice layer build as a result of this
ice pellets> 0.5cm fall to ground
produced during thunderstorms
largest hailstone recorded is 47cm diameter in south Dakota
goes up and down within the cloud fluctuating between warm and cold before allowing it to fall, it grows here

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14
Q

winter storms include combinations of

A
major snowfall 
freezing rain 
strong winds 
blowing snow
extreme wind chill
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15
Q

types of winter storms

A

ice storms
snow storm Blizzards
occur in mid to high latitudes
can result in power outages, infrastructure damage, & human health impacts

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16
Q

ice storms

A

winter storm involving at least 6.4 mm accumulation of ice
occur when a layer of warm air is between 2 layers of cold air
freezing rain

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17
Q

snow storms

A

winter storms with a large accumulation of snow

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18
Q

blizzards

A

snowstorms with:
winds > 40km/h for more than 4 hours
blowing snow that reduces visibility to 400 or less
often involve large snowfall

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19
Q

thunderstorms

A
turbulent weather accompanied by:
heavy precipitation 
lightening 
thunder 
cumulonimbus clouds 
can involve squall lines of: 
hail, strong winds, freezing ppt , tornadoes, squall line
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20
Q

squall line

A

sudden episode of high winds and thunderstorms in an area slightly ahead of an advancing cold front
occur with frequency at ITCZ (intertropical convergence zone –> low pressure band near the equator)
warms low pressure air–> air converges at surface and rises
cooling of the air resulting in condensation, hence clouds forming–> precipitation will likely occur

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21
Q

thunderstorm development

A

warm moist air rises rapidly and cools (water vapour–> water liquid= condensation)=energy is released –> local heating of the air
violent updrafts and downdraft develop

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22
Q

thunderstorm activity depends on

A

activity depends on variation of wind speed and direction (wind shear)
can produce strong winds near the ground (downbursts)

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23
Q

supercells

A

strongest type of thunderstorm
contain persistent rotating updrafts (mesocyclone)
need high wind/convection currents, warm moist air mass

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24
Q

lightning and thunderstorms

A

lightning: flashes of light caused by huge electrical discharges that superheat the air
thunder: violent expansion of heated air created by lighting which send out audible shock waves
8 million lighting strikes/day on Earth

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25
tornadoes
violently rotating column of air in contact with ground surface usually produces a visible vortex of spinning clouds and debris diameter: a few m to hundreds of km time: a few moments to tens of minutes formation: updraft from thunderstorm strong wind aloft supercell development supercell mutation Measurement: Fujita tornado scale --> measuring wind speed
26
tonado distribution
NA experiences the most tornadoes worldwide US has the most tornadoes Canada has the 2nd most tornadoes Peak months for tornadoes: May & June Tornadoes in Canada: - 80 tornadoes/year
27
continental polar (cP)
form only in the northern hemisphere most developed in the winter and cold weather cold, dense air displaces moist and warm air in its path, producing lifting, cooling, and condensation
28
an area covered by cP air in winter experiences
cold, stable air clear skies high pressure anti-cyclonic wind flow
29
Maritime Polar (mP)
occur over oceans in the Northern hemisphere an area covered by an mP air mass experiences: cool temps moist air unstable condition year round mT gulf/Atlantic unstable active from late spring to early fall mT Pacific: stable to conditionally unstable lower in moisture and energy than the mT Gulf/Atlantic
30
air mass modification
as air mass migrate from source regions, their temperature and moisture characteristics slowly take on those of the land over which they pass ex. Lake-effect snow melts of the Great Lakes
31
four atmospheric lighting mechanisms
1. convergent lifting - air flows from high to low pressure - low pressure centre: air converges, ascends, cools and condensation occurs 2. convectional lifting - air aboie a warm surface heats up - warm air rises - warmer surfaces result from local heating (ex. UHI, forest) 3. Orographic lifting - air is forced to ascend upslope as it is pushed against a mountain 4. Frontal lifting - front: leading edge of an advancing air mass line of conflict between 2 air masses
32
stationary front
a front between warm and cold air masses that is moving very slowly or not at all
33
clod fronts
- cold dense advancing air masses forces warm air upward | - warms air lifting abruptly and cools adiabatically
34
sings of cold front
``` - a few days before a cold front passes, high cirrus clouds are often observed along the leading edge of a cold front: - winds shift -temp decreases -low pressure develops -cumulonimbus clouds form -precipitation occurs ```
35
squall line:
sudden episode of high winds and thunderstorms in an area slightly ahead of an advancing cold front
36
after a cold front passes
northerly winds in N.H. temp drops high pressure develops clear skies
37
Pineapple Express
warm air carried by the jet stream from Hawaii and the pacific to the pacific coast of N.A
38
jet streams
irregular concentrated bands of westerly wind stronger in winter 300 km/hr
39
warm front
warming advancing air masses pushes air into a wedge shape and slides up and over it warm air lifts gently and cools adiabatically
40
occluded front
a composite of two fronts formed when cold front overtakes a warm front
41
cyclogenesis- stationary front
initially a stationary boundary separates warm and cool air masses
42
cyclogenesis - disturbance/wave
a disturbance triggers a wave to form within the front cold and warm air masses conflict air converges at surface air diverges aloft
43
open stage of cyclone
cyclones draw warm air from the south cyclone draw cold air from the north and west cyclone matures
44
occluded stage of cyclone
cold front wedges under warm front forming an occluded front
45
dissolving stage of cyclone
occlusion increases lifting mechanism weakens as supply of warm moist air gets cut off cyclonic system dissipates
46
tropical cyclones
cyclonic circulation originating in tropics tropical cyclones are names according to they location 80 tropical cyclones occur annually 45 per year are powerful enough to be classified as hurricanes, typhoons, and cyclones also classified according to wind speed
47
tropical cyclone terminology
hurricanes- both America typhoons - china, Japan, philippines cyclones/ tropical cyclones- Australia, India, Indonesia, Africa
48
tropical cyclone vs Midlatitude cyclone
tropical cyclones: - homogeneous air masses - high moisture - warm * leads to more powerful storms*
49
tropical cyclone anatomy
eyewall: dense wall of rain bands created as winds rush towards the centre and turn upward
50
cyclone Idai
made landfall on march 14, 2019-03-28 1.7 million people living in cyclone path in Mozambique cyclone formed in Mozambique
51
local winds
land and sea breezes | mountain and valley breezes
52
daytime valley breeze
top: high temp (lower pressure) bottom: low temp (high pressure)
53
nighttime valley breeze
top: lower temp (higher pressure) bottom: high temp (lower pressure)
54
driving Oceanic forces
``` frictional drag of wind Coriolis force density differences land configuration astronomical forces ```
55
gyres
oceanic circulation system
56
equatorial currents
currents remain near the equator due to weak Coriolis force water accumulates on eastern side of continents near the equator (western intensification) accumulated water spills northward or southward (ex. Gulf Stream & Kuroshito)
57
upwelling flows
cool, nutrients - rich water is brought upward | occurs when water is swept away from a coast
58
downwelling flows
excess water travels downward | occurs when water has accumulated as with the equatorial current
59
thermohaline circulation
deep currents resulting from differences in salinity and temperature Freshening: decrease in salt content of ocean water resulting fro freeze-thaw processes fresh water is less dense than saltwater climate change can threaten global ocean circulation patterns
60
ENSO (El Nino - southern Oscillation)
large scale ocean- atmosphere climate interaction | warmer SST in centraal and eastern Pacific affects temp & precipitation on a global scale
61
cirrostratus
formed from fused sheets of ice crystals | milky, veil - like appearance
62
cirrocumulus
while tufts with mackerel appearance | occur in lines or groups
63
fog
a cloud layer on the ground air temp and DPT @ ground level are nearly equal near ground, air is saturated for affects visibility
64
types of fog
``` radiation rime ice- crystal advection evaporation ```
65
radiation fog
``` a surface cools --> air above the surface cools air above surface reaches DPT occurs: over moist ground on clear nights does not occur over water ```
66
rime fog
``` similar process to radiation fog super-cooled water droplets often turn into frost occurs: cold weather air temp @ surface is below freezing air is moist clear skies ```
67
ice-crystal fog
air becomes full of ice crystals that forms by sublimation reduces visibility substantially occurs: low temp
68
advection fog
occurs when: warm moist air moves over cool oceans--> air cools to DPT --> advection fog warm moist air moves to higher elevations --> adiabatic cooling to DPT --> upslope fog cool dense air moves down into a valley -->valley fog
69
evaporation fog
involves advection and evaporation cold air over warm water boy water evaporates from water body moisture content of overlying air increases
70
weather vs climate
WEATHER: SHORT-TERM, DAY TO DAY CONDITION OF THE ATMOSPHERE CLIMATE: LONG TERM AVERAGE (E.G. OVER decades) of weather conditions and extremes in a region
71
elements contributing to weather
``` temp air pressure relative humidity wind speed and direction seasonal factors such as insolation ```
72
air masses
distinctive bodies of air with homogenous temp, humidity, and stability air masses initially reflects the characteristics of their source region interaction of air masses produce weather patterns
73
classification of air Masses
moisture | temp of their sources regions
74
moisture
- ''m'' for maritime (wet) | - ''c'' for continental (dry)
75
temp
``` ''A'' for arctic ''p'' for polar ''t'' for tropical ''E'' for equatorial ''AA'' for Antarctic ```
76
polar highs
frigid & dry descend and diverge clockwise or counter clockwise antarctic high is stronger than Arctic high
77
subpolar lows
cool and moist | weaker in summer, stronger in winter
78
subtropical highs
dry and hot westerlies and trade winds stronger in summer, weaker in winter
79
what direction does low pressure system air moves?
moves up
80
ITCZ Band
intertropical convergence zone energy surplus warm, low-density, low pressure air converging and rising air creating clouds
81
westerlies
prevailing surface winds flowing from subtropics to higher latitude stronger in the winter
82
jet stream
higher altitude irregular concentrated bands of westerly winds stronger in winter 300 km/ hour
83
dew point temperature
temperature at which a given mass of air becomes saturated and net condensation begins to form water droplets
84
maximum specific humidity
maximum amount of moisture possible at that specific temperature
85
explain how cyclones and anticyclones develop
Winds in an anticyclone blow just the opposite. Vertical air movements are associated with both cyclones and anticyclones. In cyclones, air close to the ground is forced inward toward the center of the cyclone, where pressure is lowest. It then begins to rise upward, expanding and cooling in the process.
86
describe regional wind patterns
At the ground level, however, the movement of the air toward the equator in the lower troposphere deviates toward the west, producing a wind from the east. The winds that flow to the west (from the east, easterly wind) at the ground level in the Hadley cell are called the Trade Winds.
87
driving forces within the atmosphere
gravitational force pressure gradient force Coriolis force friction force
88
gravitational force
Exerts virtually uniform pressure on atmosphere at Earth’s surface •Responsible for atmospheric pressure
89
pressure gradient force
* The pressure gradient results in a net force that is directed from high to low pressure and this force is called the pressure gradient force. * The pressure gradient force is responsible for triggering the initial movement of air
90
Coriolis Force
* Coriolis Force is an effect of Earth’s rotation * Deflects a moving object to the right of its moving direction in the Northern Hemisphere * Deflects a moving object to the left of its moving direction the Southern Hemisphere
91
friction force
* Friction force drags on wind at surface * Decreases with height above surface * Friction effects extend to ~ 500 m
92
2 types of local winds
land and sea breezes | mountain and valley breezes
93
evapotranspiration
the process by which water is transferred from the land to the atmosphere by evaporation from the soil and other surfaces and by transpiration from plants.
94
transpiration
is the process by which moisture is carried through plants from roots to small pores on the underside of leaves, where it changes to vapor and is released to the atmosphere.
95
Potential Evapotranspiration (POTET)
Amount of water that could evaporate and transpire given unlimited soil moisture
96
Actual Evapotranspiration (ACTET)
Evapotranspiration that occurs given a limited amount of soil water
97
trade winds
* Winds that converge at the equatorial low * Can arise form Northeast (in N.H.) or Southeast (in S.H.) * Most consistent winds on Earth
98
Hadley cells
is a global scale tropical atmospheric circulation that features air rising near the Equator, flowing poleward at a height of 10 to 15 kilometers above the earth's surface, descending in the subtropics, and then returning equatorward near the surface.
99
high level clouds include:
Cirrus, Cirruscumulus and cirrusstratus
100
In the Southern Hemisphere, the air associated with an anticyclone primarily moves:
towards the centre, counterclockwise
101
climate change
change in statistical property of the atmosphere ex. temperature
102
Hugging the ground, air mass 1 quickly approaches air mass 2. When they meet, air mass 2 to is expected to quickly lift. This can best be described as a:
occluded front