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Showing posts with label
weather [clouds]
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Showing posts with label
weather [clouds]
.
Show all posts
weather [clouds]
weather [clouds]
CLOUDS [ANIMATIONS]
cloud formation
water cycle 2
water cycle 9
29
CLOUDS [TYPES]
cirrus clouds
cumulus clouds
stratus clouds
36
51
57
47
3 types of cloud
CIRRUS
cirrus clouds
06 cirrus
09 cirrus 1
10 cirrus 2
cirrus
CUMULUS
cumulus clouds
01 alto[cumulus]
04 cirro[cumulus]
11 cumulus 1
12 cumulus 2
37
62
cumulus
stratocumulus
altocumulus
cirrocumulus
STRATUS
stratus clouds
02 alto[stratus]
05 cirro[stratus]
13 stratus 1
stratus
altostratus
30
32
33
34
42
44
45
55
54
40
38
48
49
types of clouds
Clouds form when moist air is cooled.
The main way this happens for is to force it to rise.
As warm air rises it expands because the pressure decreases with height in and this causes it to cool.
Eventually the water vapour then condenses into tiny water droplets, to those found in fog, and forms cloud.
If the temperature falls even lower, many of the cloud droplets turn to ice crystals.
There are ten main types of cloud, separated into three broad categories according to their height above the ground
LOW altitudes (cumulus or stratus),
MEDIUM altitudes (alto),
HIGH altitudes (cirrus or cirro).
Cirrus - a tuft or filament (e.g. of hair)
Cumulus - a heap or pile
Stratus - a layer
Nimbus - rain bearing
lumpy in appearance (cumuloform) or
flat (stratiform).
nimbus (rain-bearing),
castellanus (castle-like),
lenticularis (lens-shaped)
LOW altitudes (cumulus or stratus),
Low clouds are usually composed of water droplets
Stratocumulus - layered, series of rounded rolls, generally white with some shading
Stratus - layered, uniform base, grey
Cumulus - individual cells, vertical rolls or towers, flat base
Cumulonimbus - large cauliflower-shaped towers, often 'anvil tops', sometimes giving thunderstorms or showers of rain or snow
MEDIUM altitudes (alto),
Medium clouds
Medium clouds are usually composed of water droplets or a mixture of water droplets and ice crystals, and have a base between 2,000 and 5,500 metres.
Altocumulus - layered, rippled elements, generally white with some shading
Altostratus - thin layer, grey, allows sun to appear as if through ground glass
Nimbostratus - thick layer, low base, dark. Rain or snow falling from it may sometimes be heavy
HIGH altitudes (cirrus or cirro).
High clouds
High clouds are usually composed solely of ice crystals and have a base between 5,500 and 14,000 metres.
Cirrus - white filaments
Cirrocumulus - small rippled elements
Cirrostratus - transparent sheet, often with a halo
A classification of clouds was introduced by Luke Howard (1772-1864) who used Latin words to describe their characteristics.
The basis of the naming convention he developed, which we still largely use today, is whether the clouds are at :
Most of the names are also based on whether they are :
The basis of the naming convention he developed, which we still largely use today, is whether the clouds are at : LOW altitudes (cumulus or stratus), MEDIUM altitudes (alto), HIGH altitudes (cirrus or cirro). Most of the names are also based on whether they are : lumpy in appearance (cumuloform) or flat (stratiform). nimbus (rain-bearing), castellanus (castle-like), lenticularis (lens-shaped)
low clouds
Low clouds (cloud base 0-2000m) Cumulus :Low clouds (cloud base 0-2000m) These are lumpy looking clouds that can mean drastically different types of weather. Caused by columns of warm air rising and cooling, small cotton wool-like clouds (cumulus humilis) are those of a fair weather day. Cotton wool clouds over landscape Cumulus clouds that stretch further up into the sky and have a crisp cauliflower appearance (cumulus congestus) are ones that can bring intense sudden showers. Stratus:Low clouds (cloud base 0-2000m) These are low ragged looking clouds (grey or white-grey) in appearance. They often appear under rain clouds and can also be from the lifting and breaking up of fog. If thick enough they can produce drizzle or very light snow. Stratocumulus:Low clouds (cloud base 0-2000m) This is a general layer of clumpy-looking cloud that can be either white or grey in appearance depending on how thick the cloud is. This sort of cloud can appear in any type of weather situation, but when thick enough light precipitation can result. Cumulonimbus:Low clouds (cloud base 0-2000m) When one of these clouds comes along it's time to take cover! From a distance, these majestic looking clouds stretch far into the sky with the top of the clouds taking on a fuzzy anvil appearance - this is caused by ice crystals at the top of the cloud. Once under the cloud you can expect a very dark sky, torrential rain, heavy snow, hail, gusty winds or (on very rare occasions) a tornado. Mushroom shaped cloud:Low clouds (cloud base 0-2000m) One other thing to look out for on the base of the cloud are strange udder shapes. These are mammatus clouds.
medium level clouds
Medium clouds (cloud base 2000-6000m) Nimbostratus 'Dark grey and looming' can also describe the appearance of these clouds. However, unlike cumulonimbus clouds they are much more featureless, and the weather they produce isn't as severe. Instead, expect a long spell of moderate to heavy rain or snow linked to the presence of a weather front. Altostratus Another cloud that can produce rain/snow. It often appears as a bland featureless layer of cloud either ahead of, or following the passage of a weather front. If thin enough (translucidus), the sun appears as a bright disc through it. Altocumulus Formed from either columns of rising air in the medium layer of the atmosphere, or from the break-up of altostratus clouds, these generally look like clumps of cloud spread out in a layer. Occasionally they'll produce those showers that are nothing more than a few big spots of rain. Altocumulus clouds that appear like castle turrets (castellanus) can be a precursor to thunderstorms, whilst those that look like UFOs (lenticularis) are caused by air 'bouncing' over hills. Mammatus, mushroom shaped cloud:Low clouds (cloud base 0-2000m) One other thing to look out for on the base of the cloud are strange udder shapes. These are mammatus clouds. Cumulonimbus:Low clouds (cloud base 0-2000m) When one of these clouds comes along it's time to take cover! From a distance, these majestic looking clouds stretch far into the sky with the top of the clouds taking on a fuzzy anvil appearance - this is caused by ice crystals at the top of the cloud. Once under the cloud you can expect a very dark sky, torrential rain, heavy snow, hail, gusty winds or (on very rare occasions) a tornado. Stratocumulus:Low clouds (cloud base 0-2000m) This is a general layer of clumpy-looking cloud that can be either white or grey in appearance depending on how thick the cloud is. This sort of cloud can appear in any type of weather situation, but when thick enough light precipitation can result. Stratus:Low clouds (cloud base 0-2000m) These are low ragged looking clouds (grey or white-grey) in appearance. They often appear under rain clouds and can also be from the lifting and breaking up of fog. If thick enough they can produce drizzle or very light snow. Cumulus :Low clouds (cloud base 0-2000m) These are lumpy looking clouds that can mean drastically different types of weather. Caused by columns of warm air rising and cooling, small cotton wool-like clouds (cumulus humilis) are those of a fair weather day. Cotton wool clouds over landscape Cumulus clouds that stretch further up into the sky and have a crisp cauliflower appearance (cumulus congestus) are ones that can bring intense sudden showers.
high clouds
High clouds (cloud base over 6000m high) Cirrus Clouds made entirely out of ice crystals. They are white and wispy in appearance and produce no weather at the ground. Aircraft contrails (homogenitus) are a form of cirrus cloud. Cirrocumulus Made up of ice crystals and droplets of supercooled water, these are the clumpier form of cirrus clouds. The clumps are very small and can almost give the sky the appearance of fish scales. Wispy clouds Both cirrocumulus and altocumulus clouds can produce a "mackerel sky", although cirrocumulus clouds are less common. Cirrostratus Quite often the first sign in the sky of an approaching weather front, this is a uniform layer of cirrus clouds. The sun is clearly visible through these clouds, but the presence of these clouds in front of the sun can cause optical effects such as a sun halo or parhelion. Altocumulus, clouds, Altocumulus:Medium clouds (cloud base 2000-6000m) Formed from either columns of rising air in the medium layer of the atmosphere, or from the break-up of altostratus clouds, these generally look like clumps of cloud spread out in a layer. Occasionally they'll produce those showers that are nothing more than a few big spots of rain. Altocumulus clouds that appear like castle turrets (castellanus) can be a precursor to thunderstorms, whilst those that look like UFOs (lenticularis) are caused by air 'bouncing' over hills. Altostratus:Medium clouds (cloud base 2000-6000m) Another cloud that can produce rain/snow. It often appears as a bland featureless layer of cloud either ahead of, or following the passage of a weather front. If thin enough (translucidus), the sun appears as a bright disc through it. Nimbostratus:Medium clouds (cloud base 2000-6000m) 'Dark grey and looming' can also describe the appearance of these clouds. However, unlike cumulonimbus clouds they are much more featureless, and the weather they produce isn't as severe. Instead, expect a long spell of moderate to heavy rain or snow linked to the presence of a weather front.
A classification of clouds was introduced by Luke Howard (1772-1864) who used Latin words to describe their characteristics.
Cirrus - a tuft or filament (e.g. of hair)
Cumulus - a heap or pile
Stratus - a layer
Nimbus - rain bearing
The basis of the naming convention he developed, which we still largely use today, is whether the clouds are at :
LOW altitudes (cumulus or stratus),
MEDIUM altitudes (alto),
HIGH altitudes (cirrus or cirro).
Most of the names are also based on whether they are :
lumpy in appearance (cumuloform) or
flat (stratiform).
nimbus (rain-bearing),
castellanus (castle-like),
lenticularis (lens-shaped)
Clouds form when moist air is cooled to such an extent it becomes saturated.
The main mechanism for cooling air is to force it to rise.
As air rises it expands - because the pressure decreases with height in the atmosphere - and this causes it to cool.
Eventually it may become saturated and the water vapour then condenses into tiny water droplets, similar in size to those found in fog, and forms cloud.
If the temperature falls below about minus 20 °C, many of the cloud droplets will have frozen so that the cloud is mainly composed of ice crystals.
The ten main types of cloud can be separated into three broad categories according to the height of their base above the ground: high clouds, medium clouds and low clouds.
High clouds
High clouds are usually composed solely of ice crystals and have a base between 5,500 and 14,000 metres.
Cirrus - white filaments
Cirrocumulus - small rippled elements
Cirrostratus - transparent sheet, often with a halo
Medium clouds
Medium clouds are usually composed of water droplets or a mixture of water droplets and ice crystals, and have a base between 2,000 and 5,500 metres.
Altocumulus - layered, rippled elements, generally white with some shading
Altostratus - thin layer, grey, allows sun to appear as if through ground glass
Nimbostratus - thick layer, low base, dark. Rain or snow falling from it may sometimes be heavy
Low clouds
Low clouds are usually composed of water droplets - though cumulonimbus clouds include ice crystals - and have a base below 2,000 metres. Stratocumulus - layered, series of rounded rolls, generally white with some shading
Stratus - layered, uniform base, grey
Cumulus - individual cells, vertical rolls or towers, flat base
Cumulonimbus - large cauliflower-shaped towers, often 'anvil tops', sometimes giving thunderstorms or showers of rain or snow
78 clouds 1
03 High-Pressure-vs.-Low-Pressure-Weather-Diagram
17
cloud formation
cloud types
animation land sea breezes
animation of clouds
CIRRUS
cirrus clouds
06 cirrus
cloud heights
Most clouds are associated with weather. These clouds can be divided into groups mainly based on the height of the cloud's base above the Earth's surface. High Clouds: 5,000-13,000m Middle Clouds : 2,000-7,000m Low Clouds : Surface-2,000m
cloud names
naming clouds, Our language of clouds dates back to 1802, when amateur scientist and earnest sky watcher Luke Howard delivered a lecture entitled "On the Modifications of Clouds". Howard classified clouds in terms that remain familiar today: cumulus (heap), cirrus (curl), stratus (layer) nimbus (rainbearing).
CUMULUS
cumulus clouds
01 alto[cumulus]
04 cirro[cumulus]
STRATUS
stratus clouds
02 alto[stratus]
05 cirro[stratus]
08 cumulonimbus
09 cumulonimbus
10 cumulus
11 cumulus
12 kelvin_helmholtz
13 lenticular
14 nimbostratus
15 stratocumulus
16 stratus
16 clouds - altocumulus
17 clouds - altostratus
18 clouds - cirrocumulus
19 clouds - cirrocumulus
20 clouds - altocumulus
21 clouds - Cumulus congestus,towering cumulus
22 clouds - mammatus
23 clouds - cumulus humilis
24 clouds - nimbostratus
25 clouds - stratus
26 clouds - mares tails,cirrus uncinus,
27 clouds - cumulonimbus
28 clouds - stratocumulus
29 clouds - cumulonimbus
30 clouds - nimbostratus
31 clouds - stratus
32 clouds - cirrus.
33 clouds - cumulonimbus
34 clouds - cumulus
35 clouds - fog
36 clouds - altocumulus
37 clouds - altostratus
38 clouds - cirrocumulus
39 clouds - cirrostratus
40 clouds - cirrus
41 clouds - cumulonimbus
42 clouds - cumulonimbus
43 clouds - cumulus
44 clouds - cumulus
45 clouds - kelvin_helmholtz
46 clouds - lenticular
47 clouds - nimbostratus
48 clouds - stratocumulus
49 clouds - stratus
50 clouds - asperitas
51 clouds - aurora
52 clouds - cirrocumulus
53 clouds - fallstreak
54 clouds - fire in the sky
55 clouds - kelvin-helmholtz waves
56 clouds - mammatus
cols="25" rows="13">
57 clouds - nacreous
58 clouds - proton arc
59 clouds - rolling clouds
60 clouds - smokey mountains
61 clouds - virga
62 clouds - wave cloud
63 clouds - cirrus
64 clouds - cumulonimbus
65 clouds - cumulus
66 clouds - nimbostratus
67 clouds - mackerel sky
68 clouds - altocumulus
69 clouds - stratocumulus
70 clouds - nimbostratus
71 clouds - mammatus
72 clouds - fallstreak hole
73 clouds - cumulus
74 clouds - cumulus congestus
75 clouds - cumulonimbus
76 clouds - cumulonimbus
77 clouds - cirrus
78 clouds - cirrocumulus
79 clouds - cirrocumulus
80 clouds - altostratus
81 clouds - altocumulus
82 clouds - altocumulus translucidus perlucidus
83 clouds - altocumulus lenticularis
84 clouds - stratus
07 contrail
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