What is the equatorial zone known as
the tropical rain climate<\/p>\n\n\n\n
what are the Arid zones known as
the Dry Climate<\/p>\n\n\n\n
what are Warm Temperature zones known as
Mid Latitude Climate<\/p>\n\n\n\n
What is the snow zone known as
the sub-artic climate<\/p>\n\n\n\n
what is the polar zone known as
the snow climate<\/p>\n\n\n\n
location of tropical rain climate
10 degrees either side of the equator<\/p>\n\n\n\n
temperature in tropical rain climate
highs up to 35 degrees, lows down to 20 degrees<\/p>\n\n\n\n
humidity in tropical rain climate
high humidity and convective weather<\/p>\n\n\n\n
is there a dry season in tropical rain climate
no<\/p>\n\n\n\n
winds in tropical rain climate
light winds<\/p>\n\n\n\n
classification of tropical rain climate
monsoonal<\/p>\n\n\n\n
tropical savannah climate boundary
10-25 degrees of latitude<\/p>\n\n\n\n
temperature in savannah climate
high with mean temperature above 18 snd diurnal and seasonal variation increasing with latitude<\/p>\n\n\n\n
rain in savannah climate
wet in summer and dry in winter with the wet season associated with the overhead sun<\/p>\n\n\n\n
winds in savannah climate
dry trade winds in winter<\/p>\n\n\n\n
Dry climate subdivisions
Desert and Steppe<\/p>\n\n\n\n
How do steppe and desert regions differ
steppe regions are wetter and have more vegetation<\/p>\n\n\n\n
Pressure in dry climate
high<\/p>\n\n\n\n
temperature in dry climate
very hot with large daily and seasonal variations<\/p>\n\n\n\n
precipitation in dry climate
on equatorial side in summer and on polar side in winter<\/p>\n\n\n\n
winds in dry climate
prevalent trade wind<\/p>\n\n\n\n
winds in cool mid latitude climate
predominant westerly winds and passage of frontal depressions<\/p>\n\n\n\n
is there a dry season in a cool mid latitude climate
no<\/p>\n\n\n\n
are there seasonal variations in a cool mid latitude climate
yes<\/p>\n\n\n\n
mid latitude climate in warm temperate zone
transition climate<\/p>\n\n\n\n
transitional climate
significant variations due to the seasonal position of the sun<\/p>\n\n\n\n
winter conditions in warm mid latitude climate
similar to cool temperate zone<\/p>\n\n\n\n
summer conditions in warm mid latitude climate
associate with arid zone<\/p>\n\n\n\n
conditions in sub-artic climate
cold dry winter and hot summer<\/p>\n\n\n\n
seasonal variation is Snow Climate
Extreme seasonal variation<\/p>\n\n\n\n
winter in snow climate
extremely cold<\/p>\n\n\n\n
why is the ITCZ further away from the equator over land masses
land warms quicker<\/p>\n\n\n\n
Mesoscale Convective System
complex thunderstorms on larger scale than individual ones that can last for several hours or more<\/p>\n\n\n\n
where are MCS found
ITCZ<\/p>\n\n\n\n
Why is ITCZ referred to as doldroms
lack of horizontal air movement due to convective activity<\/p>\n\n\n\n
Monsoon
seasonal changes in circulation and precipitation caused by the asymmetric heating of land and sea masses<\/p>\n\n\n\n
monsoon in India is summer
south west winds brings in warm moist air from sea and heavy precipitation<\/p>\n\n\n\n
monsoon in India in winter
North east Monsoon with drier air<\/p>\n\n\n\n
Where is affected by Monsoon winds
India, coastal areas of Africa, regions of North America and Chile<\/p>\n\n\n\n
ITCZ in summer
very moist air from Atlantic combined with thermal and convergent uplift produces significant precipitation in northern Africa<\/p>\n\n\n\n
Harmattan
hot dry wind that picks up sand from Sahara along its fetch which can cause significant reductions in visibility<\/p>\n\n\n\n
harmattan in winter
can be quite cool<\/p>\n\n\n\n
Weather over East Asia in winter
north easterly flow driven by Siberian high<\/p>\n\n\n\n
weather is East Asia in summer
significant precipitation associated with the Monsoon in July and August due to warm moist Pacific Air drawn over continent<\/p>\n\n\n\n
What is Australian summer monsoon driven by
strong heat lowers over Northern Australia<\/p>\n\n\n\n
Monsoonal flow in Northern Australia
not as strong or steady as the Indian Monsoon<\/p>\n\n\n\n
Onset of monsoonal flow in Northern Australia
occurs during January<\/p>\n\n\n\n
what happens as southeast Asian winter monsoon strengthens
flow penetrates deeper into tropical latitudes crossing equator and turning westerly until April with the return of easterly trade winds<\/p>\n\n\n\n
Easterly waves
troughs of low pressure that flow from east to west<\/p>\n\n\n\n
what can easterly waves cause
disturbed weather along ICTZ and hurricanes<\/p>\n\n\n\n
easterly waves cased by
african easterly jet which is large scale sea breeze<\/p>\n\n\n\n
African easterly jet
removes air over the Atlantic off the West Africa Coast and low pressure area formed is a trough producing convective weather and thunderstorm activity<\/p>\n\n\n\n
what is mid latitude weather influenced by
position of polar front<\/p>\n\n\n\n
how do depressions produced by the polar front travel
west to east<\/p>\n\n\n\n
where are westerly winds in mid latitudes produces
high pressure regions in the sub tropical belt<\/p>\n\n\n\n
westerly winds in the southern hemisphere
very fast as little land mass to impede process so they are referred to as the roaring forties<\/p>\n\n\n\n
Location of the Mistral
flows south down the Rhone Valley and out into the Gulf of Lyons<\/p>\n\n\n\n
what is associated with the Mistral
genoa low in the gold of Gulf of Genoa<\/p>\n\n\n\n
when does the Mistral occur
airflow through the Rhone Valley is enhanced when an area of high pressure lies to the west and a polar front depression to the east<\/p>\n\n\n\n
what airstream feeds the Mistral
polar maritime<\/p>\n\n\n\n
what makes the Mistral faster
katabatibc winds and fuelling effects<\/p>\n\n\n\n
Mistral speed
in excess of 75kts<\/p>\n\n\n\n
Where does the Bora occur
blown down Dynamic coastal mountain range<\/p>\n\n\n\n
when does Bora occur
when there is high pressure over central europe and the balkans and low pressure over the med<\/p>\n\n\n\n
what causes Bora to be so strong
Katabatic effect<\/p>\n\n\n\n
what speeds can Bora reach
70kts with gusts in excess of 100kts<\/p>\n\n\n\n
What is the Scirroco
hot, dry dusty wind that blows from North Africa across the med<\/p>\n\n\n\n
Other names for the Scirroco
Chilli, Ghibli and Khamsin<\/p>\n\n\n\n
What causes Scirroco
blows easterly due to depressions transiting the Mediterranean<\/p>\n\n\n\n
max speed of Scirroco
around 55kts<\/p>\n\n\n\n
weather caused by Scirroco
moisture picked up from med can cause low cloud and drizzle<\/p>\n\n\n\n
When does Fohn wind occur
when air in horizontal motion meets a significant mountain range and it is forced over the top<\/p>\n\n\n\n
weather caused by Fohn wind
cloud due to the air adiabatically cooling at the DALR and then the SALR and warms as it descends<\/p>\n\n\n\n
why does Fohn wind warm Lee side of mountain
air cools less at SALR and more at DALR<\/p>\n\n\n\n
Where does the name Fohn wind come from
local wind in the alps<\/p>\n\n\n\n
Chinnok
name for Fohn wind in Rockies<\/p>\n\n\n\n
where can outbreaks of polar air reach
sub tropical latitudes – below 30N<\/p>\n\n\n\n
what can outbreaks of polar air cause
unseasonably cold weather and snowfall between 30-50N<\/p>\n\n\n\n
Blizzard
polar air outbreaks in northern hemisphere<\/p>\n\n\n\n
Pampero
polar air outbreaks in southern hemisphere<\/p>\n\n\n\n
what causes polar air outbreaks
cooler air descending and cooling at polar caps reaches critical mass and breaks away<\/p>\n\n\n\n
cold air pool
deep cold core aloft which is undetectable at ground level<\/p>\n\n\n\n
what causes cold air pools
left over from polar air outbreak<\/p>\n\n\n\n
cold air pool conditions
unstable due cold air on top of warm moist air<\/p>\n\n\n\n
what causes cold air pool conditions to dissapate
dissipation of cold air pool itself<\/p>\n\n\n\n
lifespan of cold air pool
several days<\/p>\n\n\n\n
diameter of cold air pool
300nm-600nm<\/p>\n\n\n\n
vertical extent of cold air pool
10000ft to 30000ft<\/p>\n\n\n\n
where do cold air pools appear over Europe
behind cold front7<\/p>\n\n\n\n
Untrue about the Tropopause
Temp starts to fall serverly above tropopause<\/p>\n\n\n\n
The tropopause breaks are important for aviation because
The cores of jet streams can be located near these breaks<\/p>\n\n\n\n
At North Atlantic Lat of 50 deg in winter the height of the tropopause is approximately
31000 ft ie average height 16km x cos(lat)<\/p>\n\n\n\n
Majority of ozone found
In stratosphere relatively high round 30km<\/p>\n\n\n\n
Lowest layer of the atmosphere
Troposphere<\/p>\n\n\n\n
The inversion in the lower troposphere created by old H psi system during day or night
Subsidence inversion<\/p>\n\n\n\n
The 2 most important methods of heat transfer from surface to higher levels of the troposphere
Formation of convection clouds and long wave radiation<\/p>\n\n\n\n
During a valley inversion
Over night cool dense air as a result of radiation cooling will descend along mountain slopes into the basin and lest to the development of a valley inversion<\/p>\n\n\n\n
A significant inversion at low height is a characteristic of
Nocturnal radiation<\/p>\n\n\n\n
On a clear sky in summer, continental ground surface, wind calm the minimum temperature is reached approximately
Half an hour after sunrise (30 min after sunrise)<\/p>\n\n\n\n
The primary cause of all changes in the Earth’s weather is
Is variation of solar energy received by the earth surface<\/p>\n\n\n\n
1.98 deg c per
1000 ft<\/p>\n\n\n\n
0.65 deg c per
100m<\/p>\n\n\n\n
Frequency band of Wx radar
8-12GHz<\/p>\n\n\n\n
wavelength of wx radar
2.5-4cm<\/p>\n\n\n\n
Ts avoidance
20nm above FL200 and 10nm below FL200<\/p>\n\n\n\n
Hadley cells
series of rising and descending cell circulations<\/p>\n\n\n\n
air in equatorial regions
rises due to surface heat and diverges at higher levels and then sinks cause sub-tropical high pressure belts<\/p>\n\n\n\n
Surface air rotation around the sub tropical highs
cause trade winds through Coriolis force<\/p>\n\n\n\n
Air rising on the polar front
caused by air from sub-tropical highs meeting polar air and forms polar front depressions<\/p>\n\n\n\n
wladimir koppen
classified climates based on vegetation<\/p>\n\n\n\n
equatorial zone
also known as the tropical rain climate between 10S and 10N<\/p>\n\n\n\n
equatorial zone sub zones
tropical rain forest and tropical savannah<\/p>\n\n\n\n
conditions in tropical rain forest
high temperature up to 35 degrees with little seasonal variation, no dry season, light winds, high humidity and high amount of convective weather<\/p>\n\n\n\n
location of tropical savannah
10 to 25N and S<\/p>\n\n\n\n
conditions in tropical savannah
high mean temperature of 18 degrees, increasing diurnal and seasonal variation with latitude, wet in summer and dry in winter with dry trade winds in winter<\/p>\n\n\n\n
Arid zone
AKA dry climate with 2 zones<\/p>\n\n\n\n
zones of arid zone
steppe climate and desert climate<\/p>\n\n\n\n
conditions in arid zone
high pressure, hot in summer with large diurnal and seasonal variations, precipitation in summer on equatorial side and polar side in winter, prevalent trade wind<\/p>\n\n\n\n
temperate zone
AKA mid latitude climate split into the warm and cold temperate zones<\/p>\n\n\n\n
characteristics of warm temperate zone
westerly wind aiding the passage of frontal depressions, no dry season and seasonal variations, a transitional climate<\/p>\n\n\n\n
what causes warm summer in transitional climate
sub tropical highs which are associated with the arid zone<\/p>\n\n\n\n
snow zone
aka sub-artic climate covering areas of continental North America, Scandinavia, and former USSR<\/p>\n\n\n\n
conditions in snow zone
cold dry in winter and hot in summer with average temperature of 0<\/p>\n\n\n\n
polar zone
aka snow climate, extreme season variation, extreme cold winters and period of constant dark and light<\/p>\n\n\n\n
ICTZ further from equator over land masses
land masses are warmed more quickly than sea<\/p>\n\n\n\n
northeast trade winds
converge in a low pressure zone creating ITCZ<\/p>\n\n\n\n
solar heating in ITCZ
forces air to rise through convection and leads to unstable conditions combined with high lapse rates<\/p>\n\n\n\n
mesoscale convective system
triggered by ITCZ, complex of thunderstorms and larger scale, lasting longer<\/p>\n\n\n\n
wettest zone on earth
equatorial zone with 200 days of precip per year<\/p>\n\n\n\n
monsoon
seasonal changes caused by asymmetric heating of the land masses<\/p>\n\n\n\n
cause of windshift with monsoon
differential in surface heating between the land and the sea<\/p>\n\n\n\n
southwest monsson
affects in summer with warm moist air and precip<\/p>\n\n\n\n
Pressure system with SW monsoon affecting Inda
low over Pakistan<\/p>\n\n\n\n
north east monsoon
affect in winter with a much drier air mass<\/p>\n\n\n\n
pressure systems with north east monsoon affecting India
high over Tibet<\/p>\n\n\n\n
places experiencing monsoon other than Inda
Northern Australia, coastal Africa, North America and Chile<\/p>\n\n\n\n
monsoon of western sub-saharan Africa
due to temperature and humidity difference between Sahara and Atlantic and shift of ITCZ<\/p>\n\n\n\n
August in western sub-saharan Africa
ITCZ north over Sahara, moist air from Atlantic blows in causing thermal and convergent uplight causing significant precip<\/p>\n\n\n\n
January in sub-saharan Africa
ITCZ further south, very hot and dry and NE trade winds cause Harmattan<\/p>\n\n\n\n
Harmattan
Very hot dry wind blowing between November and April that can cause dust and sandstorms up to FL150<\/p>\n\n\n\n
East Asia Monsoon
Cold north easterly flow in winter driven by the Siberian Highs and a warm moist south westerly flow in summer driven by Asian low causing significant precip<\/p>\n\n\n\n
ITCZ in winter
moves south and lies over Indonesia and northern Australia<\/p>\n\n\n\n
Siberian high
lies over Asia in winter<\/p>\n\n\n\n
Australia Summer monsoon
driven by strong heat lows like Asian monsoon, not as strong or steady as Indian monsoon, and penetrates into the tropical latitudes as it strengthens<\/p>\n\n\n\n
when does the Australian summer monsoon happen
January<\/p>\n\n\n\n
trade winds in Jan
cross equator near Indonesia and turn westerly flowing across northern Australia<\/p>\n\n\n\n
how long does Australian summer monsoon last
until the easterlies return<\/p>\n\n\n\n
easterly waves
disturbed weather along ITCZ that travel east to west<\/p>\n\n\n\n
what are easterly waves
troughs of low pressure south of the azores high generated by the african easterly jet<\/p>\n\n\n\n
african easterly jet
removes air over atlantic forming low pressure area which forms trough causing convective weather, blows generally in summer<\/p>\n\n\n\n
mid latitude weather
influenced by the position of the polar front and makes westerly depressions<\/p>\n\n\n\n
pressure systems in winter
migrate southwards like the ITCZ<\/p>\n\n\n\n
Mistral
flows south down the Rh\u00f4ne valley into the Gulf of Lyons, mainly in winter months due to the prevalent pressure systems<\/p>\n\n\n\n
pressure systems associated with Mistral
Genoa low<\/p>\n\n\n\n
what enhances the Mistral
high pressure to the west and polar front depression to the east<\/p>\n\n\n\n
what often feeds the mistral
maritime air masses<\/p>\n\n\n\n
what fuels the mistral
katabatic winds<\/p>\n\n\n\n
mistral strength
up to 75kt can last several days<\/p>\n\n\n\n
Bora
blows down the Dinaric mountain range in winter<\/p>\n\n\n\n
pressure systems for the Bora
high pressure over central europe and low pressure over the med<\/p>\n\n\n\n
strength of Bora
cold and gusty averaging 70kts helped on with katabatic winds<\/p>\n\n\n\n
Scirocco
Hot, dry and dusty winds from north africa across the Med<\/p>\n\n\n\n
scirocco also known as
Chilli, ghiblii, Khamsin<\/p>\n\n\n\n
when is the scirocco easterly
when produced by depressions crossing the med<\/p>\n\n\n\n
max speed of scirocco
55kt<\/p>\n\n\n\n
weather with scirocco
low cloud and drizzle with the moisture picked up from the med<\/p>\n\n\n\n
F\u00f6hn wind
air meeting mountain range forced up and cooled adiabatically forming cloud if cooled below dew point<\/p>\n\n\n\n
warming with F\u00f6hn wind
up to 10 degrees on Leeward side<\/p>\n\n\n\n
Polar air outbreaks
can reach subtropical regions down to 30N\/S bringing unseasonably cold weather<\/p>\n\n\n\n
snow fall from polar air outbreaks
between 30N-50N as cold air mixes with warm air<\/p>\n\n\n\n
other names for polar air outbreaks
blizzard in northern hemisphere and pamper in southern hemisphere<\/p>\n\n\n\n
formation of polar air outbreak
cooling, descending air reaches critical mass and breaks away from the polar air mass<\/p>\n\n\n\n
cold air pool
deep, cold core aloft undetectable at ground level<\/p>\n\n\n\n
what is a cold air pool made of
remaining cold air from polar air outbreak<\/p>\n\n\n\n
cold air pool over warm moist air
unstable conditions can produce area of convective cloud<\/p>\n\n\n\n
when does a cold air pool dissipate
after mixing<\/p>\n\n\n\n
life span of cold air pool
up to several days<\/p>\n\n\n\n
dimensions of cold air pool
300nm-600nm in diameter from FL100 to FL300<\/p>\n\n\n\n
where to cold air pools tend to form
half of them behind cold front and are difficult to predict<\/p>\n\n\n\n
Land and sea breezes
produced by pressure differential cased by temperature difference – pressure differential can cause change by 500ft to 1000ft<\/p>\n\n\n\n
Sea breezes
tend to form in afternoon and produce fall in temperature and increase in humidity<\/p>\n\n\n\n
effects of sea breeze
felt up to 1000ft, 10-15nm either side of the coast line and can cause small cumuliform clouds<\/p>\n\n\n\n
strength of sea breeze
up to 10kt and deflected to the right in the northern hemisphere<\/p>\n\n\n\n
anabatic winds
slope heated and air is warmed through conduction causing air to be less dense and rise and is not usually noticeable due to irregular topography<\/p>\n\n\n\n
what can energise anabatic winds
funnel feature of valley<\/p>\n\n\n\n
katabatic winds
slope cools, cooling the air through conduction, air is denser and sinks and can cause formation of fog and mist<\/p>\n\n\n\n
when are katabatic winds commonly found
at night<\/p>\n\n\n\n
example of katabatic winds
Bora to an extent and can blow during daylight hours due to the cooling effect of the land in winter<\/p>\n\n\n\n
what enhances the bora
funnel affect of topography and prevailing pressure systems<\/p>\n\n\n\n
ravine or valley wind
generally follows the contours if the atmosphere is stable<\/p>\n\n\n\n
when is a ravine or valley wind subject to the venturi effect
when the valley is aligned in the general direction of the wind<\/p>\n\n\n\n
example of ravine or valley wind
Mistral<\/p>\n\n\n\n
headland effect
wind blowing parallel to coast and headland squeezes isobars increasing the pressure gradient and windspeed<\/p>\n\n\n\n
when does the f\u00f6hn wind cause more heating
when more water is deposited<\/p>\n\n\n\n
conditions for mountain waves
wind 30 degrees either side of normal to mountains increasing with height with little variation on the same heading, and stable layer of atmosphere with less stable atmosphere above<\/p>\n\n\n\n
windspeed for mountain waves
15kt at crest<\/p>\n\n\n\n
wavelength of mountain wave =
knots\/7<\/p>\n\n\n\n
mountain wave in stratosphere
caused by irregular features near initiation mountains and are of greater length than those in the troposphere<\/p>\n\n\n\n
double amplitude of mountain waves
1500ft up to 1000fpm Vertical Speeds<\/p>\n\n\n\n
Lenticular clouds
form in the stable layer of the standing wave<\/p>\n\n\n\n
rotor clouds
Ragged Cu or Sc, parallel to downwind ridge rotating about the horizontal axis<\/p>\n\n\n\n
number of rotors
1 or 2<\/p>\n\n\n\n
Cap clouds
usually form on the ridge crest an can be extended by strong winds to create a f\u00f6hn wall but can be obscured by frontal clouds<\/p>\n","protected":false},"excerpt":{"rendered":"
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