chapter10-12 Flashcards
Thermal local winds that occur in the ___________ during the warmer part of the year create Sea, Land, Mountain, Valley and Slope Breezes occur primarily because of ________ cooling and heating
MIDDLE LATITUDES
RADIATIONAL
Thermal local winds that depend on radiational cooling and heating are tied closely to the ________
TIME OF DAY
A Sea Breeze refers to a local wind that flows from the ___ to the ____. Sea Breezes occur because the _______ of the land surface increases more rapidly than the temperature of the surface of the ___
SEA to the LAND
TEMPERATURE
SEA
The Sea Breeze is also accompanied by a very slight change in atmospheric ______which aids wind movement. A well-developed Sea Breeze will have winds of ________ will extend from the _____ up to as high as _____. above the surface.
PRESSURE
10 to 20 knots
SURFACE
3,000 FT
Above the Sea Breeze the wind will move back toward the sea creating a local circulation of low altitude winds flowing toward ______ with slightly higher altitude winds at about 6,000 feet flowing towards ______ which completes the Sea Breeze Circulation.
THE LAND
THE SEA
A Sea Breeze describes ____air moving inland from the sea. Air movement occurs because the ____heats more rapidly than the sea and warm air rising over the land. Heating reduces pressure which creates a _______pressure gradient (very small gradient) creating enough difference to generate air movement
COOL
LAND
HORIZONTAL
A Sea Breeze Front may develop along with the Sea Breeze. The Sea Breeze Front may be marked by a broken line of _______clouds. If sufficient instability exists, the Sea Breeze Front may be marked by a line of ________.
CUMULOUS
THUNDERSTORMS
Thermal winds are normally named for the _____ of the breeze and flow from _____to warm
SOURCE
COLD
Sometimes, due to a Sea Breeze Front (very localized, very narrow), the _____ sea breeze forces warmer land-side air aloft which sometimes creates lower altitude _____ clouds at about 2,000’ – 3,000’
COOLER
CUMULOUS
Sometimes, sea breezes will flow around _____ near the coastlines and create convergence zones. A good local example is the flow around the Olympic Mountains which creates a _____zone in the vicinity of Seattle.
TERRAIN
CONVERGENCE
Land Breezes occur a few hours after ____ due to the more rapid cooling of the surface of the land compared to the surface of the ___, and work very much like the Sea Breeze except the circulation flows at low altitude toward the ___ and at higher ______toward the land
SUNSET
SEA
SEA
ALTITUDE
Generally, a Land Breeze will be weaker than a _______ with winds of only about 5 knots and with the overall circulation only extending up to about ____ FEET
SEA BREEZE
2,00 FEET
A Valley Breeze is a circulation of air toward higher _____ that creates air that flows upslope, and has a corresponding circulation of air that flows out from the mountains at higher altitudes and then descends over the ______. The term for an upslope wind is ______
TERRAIN
LOWLANDS
ANABATIC
An Anabatic wind occurs because the air in the vicinity of ________ heat ____ than the air at the same altitude over lower elevations and the differential heating creates a very small differential ______ change which creates the wind flow.
MOUNTAIN SLOPES
FASTER
PRESSURE
Upslope and Valley Breezes usually reach maximum speeds during the middle of the _______with speeds of 5 to 20 knots. Because snow cover tends to reflect rather than absorb solar radiation, snow cover tends to reduce the effects of _____ and _____ breezes.
AFTERNOON
UPSLOPE
VALLEY
Mountain Breezes occur primarily at _____ as the cooler air at higher altitude near the surfaces of mountain slopes cools more _____ than air at the same altitude over lower elevations. The term for down-slope winds is ______.
NIGHT
RAPIDLY
KATABATIC
Mountain Breeze ______wind circulation works in reverse from the Anabatic winds of the ______Breeze. In a Katabatic circulation warmer air at altitude from over lower elevations flows toward ______ slopes
KATABATIC
VALLEY
MOUNTAIN
Cold Downslope or Drainage winds occur when cold dense air sinks and strengthens ______ and ______breezes
DOWNSLOPE
MOUNTAIN
Mountain Lee Waves and Warm, Downslope winds are ______wave patterns that develop over and ______of mountains. These two winds are forms of Atmospheric ______ Wave air movement
MESOSCALE
DOWNWIND
GRAVITY
Mountain Lee waves occur in movement of _____air over mountains with a wind speed of at least __ knots and may persist for several ____. The danger of a Mountain Lee wave wind is that on the Lee side, the air can be very ______.
STABLE
20 KN
HOURS
TURBULENT
A weak Lee Wave will have vertical movement of a few hundred ____. A strong Lee Wave can have vertical movement of up to ____feet per minute and can attain vertical changes of up to ____ feet or more.
FEET
1800 FEET
4000 FEET
Two locations where Mountain Lee Waves are strongest are the lee slopes of the _________ in California and the ________ in Colorado
SIERRA NEVADA RANGE
ROCKY MOUNTAINS
Indications of potential Mountain Lee wave action are ______Clouds (lens-shaped clouds) that will occur above the peaks of the mountain range and downwind of the Mountain range when wind speeds exceed ___knots and the direction of wind flow is ________ to the mountain ridgelines
LENTICULAR
20 KNOTS
PERPENDICULAR
Examples of Warm Downslope winds and where they occur A. B. C. D. E.
a. CHINOOK WINDS - EAST SLOPES OF THE ROCKY MOUNTAINS
b. FOEHN WINDS - NORTHERN SLOPES OF THE ALPS
c. SANTA ANA WINDS - SOUTHERN CALIFORNIA
d. CANTERBURY NOR’WESTER - NEW ZEALAND
e. MONO WIND – CENTRAL AND NORTHERN CALIFORNIA
Wind shear is a change of wind speed of direction in a very ______
SHORT DISTANCE
Low level wind shear magnitude change of 8 to 11 knots is considered Strong and ____________ is considered severe.
12 KNOTS OR MORE
A METAR report that reads /RMK LLWS -15KT SFC to 030 DURC means the wind shear resulted in a loss of _______ during climb-out between the _____and ____.
AIRSPEED OF 15 KNOTS
SURFACE
3,000FT