国产男女无遮挡_日本在线播放一区_国产精品黄页免费高清在线观看_国产精品爽爽爽

  • 熱門標(biāo)簽

當(dāng)前位置: 主頁 > 航空資料 > 飛行資料 >

時(shí)間:2010-05-30 00:10來源:藍(lán)天飛行翻譯 作者:admin
曝光臺(tái) 注意防騙 網(wǎng)曝天貓店富美金盛家居專營店坑蒙拐騙欺詐消費(fèi)者

If the wind increases to 10 kts, what
can you expect when you arrive?
9. A TAF time group of 0220 means
what?
10. A VOLMET report for 0500
UTC in the Autumn gives a surface
wind of 5 kts, temperature of 9°C,
dewpoint of 8°C and 1500m
visibility, with no cloud reported. If
you plan to arrive at 0600, what
weather can you expect?
Weather 111
11. What do these parts of a TAF
mean?
0615 15030G401200 BR
SCT008
12. And these?
TEMPO 1420 8000 SHRA
PROB30 TEMPO 1415 5000
13. On a calm, clear evening, the
METAR for the destination contains
the figures 04/03. What can you
expect on arrival?
14. What is QFF?
15. Define Density.
16. Define Dewpoint.
17. What is the SALR?
18. What is a gust? A squall?
19. At what height is the geostrophic
wind?
20. What is an isallobar?
21. What is an anabatic wind?
22. What might you expect from a
thunderstorm?
23. What might you expect from
icing?
Some Answers
1. ISA 0°C, -13°C, FL 280, ISA -
5°C, +14°C, FL 140.
2. The difference between the
altimeter setting and 1013.2 mb
(29.92") is 24 mb, a difference of 720
feet, so the PA of the high ground is
6600 feet. Subtract this from 10,000
feet for 3400 feet clearance.
3. 29.38 from 29. 92 is .54, or 540
feet, so the PA of your aircraft is
3040 feet. The separation is
therefore 460 feet.
4. The answers in order:
·  At 2000 feet, wind is
unaffected by surface friction.
With no drift, you are parallel
to the isobars and true
altitude is constant.
·  True altitude is decreasing,
because the 500-foot wind is
backed with reference to the
wind at 2000 feet, and you are
crossing the isobars from
high to low pressure because
of the drift you have to apply.
5. Wind speed will reduce by about
20%, so the coriolis effect will
automatically reduce by about 20°.
Thus, 360-20 is 340°, and 20% of 15
is 3, so the speed will be 12 kts.
6. At first sight, it would be 18, but
in late afternoon, the Coriolis effect
could well make it 21.
7. The airframe is cold, as you are
below freezing. You will therefore
most likely get clear ice.
8. Thin low stratus cloud.
9. It is valid between 2 in the
morning and 8 at night.
10. As the wind is light, and the
temperature is very close to the
dewpoint, you are very likely to see
radiation fog, because there is no
cloud and it is very near dawn. The
visibility is already poor, and will get
worse, before possibly clearing by
mid-morning after solar heating.
Note that the minimum RVR for a
visual approach is 800m.
11. Valid between 6 in the morning
and 3 in the afternoon (UTC, of
course), the wind is from 150° at 30
kts, gusting 40, visibility 1200 metres
in mist. 3-4 oktas of cloud at 800'.
112 JAR Private Pilot Studies
12. Temporarily between 1400 and
2000, 8000m visibility in showers
and rain. 30% probability of a
temporary reduction in vis to 5000m
between 1400 and 1500.
13. The temperature is 4°C and the
dewpoint 3°C, meaning that, if the
temperature falls, as it is likely to if it
is calm and clear, moisture will
condense out and form mist or fog.
14. The QFE reduced to mean sea
level pressure using the ambient
temperature lapse rate. It gives a
more accurate estimation of sea level
pressure and is used when producing
surface weather charts.
15. Mass per unit volume.
16. The temperature to which air
must be cooled, without change of
pressure, for the air to just become
saturated. Any further cooling results
in condensation.
17. The Saturated Adiabatic Lapse Rate
is the rate at which a parcel of
saturated air changes temperature
with height.
18. Temporary increases in
prevailing windspeed. A squall is
normally associated with
thunderstorms and lasts longer.
19. Around 2000 feet.
20. A line joining points of equal rate
of change of pressure.
21. The reverse of a katabatic wind,
flowing uphill (at a slower pace).
22. Hail, icing, lightning, static
electricity, turbulence and windshear.
23. More weight, less lift, more drag,
stuck controls, less visibility, radio
interference and blockages.
Electricity & Radio
Radio depends on the movement of
electric and magnetic waves, which
depend on the movement of
electricity, which ultimately depends
 
中國航空網(wǎng) www.k6050.com
航空翻譯 www.aviation.cn
本文鏈接地址:JAR.Private.Pilot.Studies(74)
国产男女无遮挡_日本在线播放一区_国产精品黄页免费高清在线观看_国产精品爽爽爽
北条麻妃99精品青青久久| 手机看片福利永久国产日韩| 亚洲一区二区三区欧美| 成人久久精品视频| 亚洲日本精品国产第一区| 国产精品av在线播放 | 欧美日韩成人黄色| 国产老熟妇精品观看| 亚洲精品无码久久久久久| 91久久国产精品| 日韩欧美一区二区三区四区五区 | 久久99九九| 国模吧一区二区| 亚洲一区二区三区四区视频| 久久久久资源| 国产日韩欧美精品| 无码人妻精品一区二区三区66| 久久久久久久久综合| 国产在线精品成人一区二区三区| 亚洲欧洲日本国产| 日韩亚洲成人av在线| 国产日本在线播放| 午夜精品久久久久久久白皮肤| 久久久久久中文字幕| 国产日韩一区欧美| 日本在线观看a| 国产精品海角社区在线观看| 97精品国产97久久久久久粉红| 欧美一级黄色网| 久久亚洲私人国产精品va| 91精品成人久久| 黄色网在线视频| 亚洲精品第一区二区三区| 国产精品私拍pans大尺度在线| 欧美激情精品久久久久久蜜臀| 奇米影视首页 狠狠色丁香婷婷久久综合 | 日本高清不卡一区二区三| 欧洲久久久久久| 日韩在线观看网址| 国产精品一区二区三| 欧美性视频在线播放| 亚洲色成人一区二区三区小说 | 欧日韩在线观看| 亚洲自拍中文字幕| 国产精品入口免费视频一| 99久久免费国| 国精产品99永久一区一区| 日本高清久久一区二区三区| 中文字幕一区二区三区有限公司 | 欧美一级爱爱| 日韩中文字幕av在线| 国产aaa精品| 国产精品日韩欧美综合| 久久国产手机看片| 91精品久久久久久久久中文字幕| 蜜臀精品一区二区| 欧美中文娱乐网| 亚洲在线观看一区| 久久伊人精品一区二区三区| 久草综合在线观看| 国产精品a久久久久久| 日本一区二区三区四区五区六区| 精品不卡一区二区三区| 国产成人免费高清视频| 国产一区二区高清视频| 欧美日韩一区在线视频| 青青青国产在线观看| 日产精品久久久一区二区 | 91免费国产视频| 国产精品午夜国产小视频| 麻豆成人av| 国语自产精品视频在线看一大j8| 人妻无码久久一区二区三区免费 | 国产精品免费区二区三区观看| 国产成a人亚洲精v品在线观看| 91精品国产沙发| 超碰国产精品久久国产精品99| 国产偷人视频免费| 国产特级黄色大片| 国产日韩精品综合网站| 国产亚洲欧美一区二区三区| 精品视频免费在线播放| 黄www在线观看| 免费久久久久久| 欧美亚洲精品一区二区| 欧美专区在线视频| 欧美亚洲免费高清在线观看| 欧美专区福利在线| 欧美污视频久久久| 欧美日韩精品一区| 欧美日韩一区在线播放| 黄色免费视频大全| 每日在线更新av| 国产女同一区二区| 国产精品一区而去| 成年人网站国产| 91国产高清在线| 久久av免费一区| y97精品国产97久久久久久| 国产成人一区二区三区电影| 国产激情一区二区三区在线观看 | 日本一区二区三区视频在线播放| 日本特级黄色大片| 欧美这里只有精品| 精品日本一区二区| 国语自产精品视频在线看| 国产午夜福利在线播放| 国产美女在线精品免费观看| y111111国产精品久久婷婷| 116极品美女午夜一级| 久草在在线视频| 国产精品久久久久91| 欧美精品日韩三级| 亚洲三区在线| 品久久久久久久久久96高清| 精品一区二区成人免费视频| 国产伦精品一区二区三区视频免费 | www亚洲国产| 久久免费视频网| 久久精品91久久香蕉加勒比 | 国产视频一区二区视频| 99超碰麻豆| www.日本久久久久com.| 久久国产精品亚洲| 少妇av一区二区三区无码| 欧美精品成人一区二区在线观看| 国产美女精品视频免费观看| 国产精国产精品| 国产精品毛片a∨一区二区三区|国 | 亚洲一区二区三区乱码| 日韩精品在线观看av| 国产一区二区在线免费| 久久久免费观看| 久久香蕉频线观| 性色av香蕉一区二区| 蜜桃久久精品乱码一区二区| 91久久国产婷婷一区二区| 久久精视频免费在线久久完整在线看| 色综合久久精品亚洲国产| 亚洲二区三区四区| 僵尸世界大战2 在线播放| 国产精品亚洲天堂| www.美女亚洲精品| 亚洲一区二区精品在线| 欧美精品一区二区三区在线看午夜 | 国产精品视频自拍| 国产精品免费一区二区三区观看| 国产精品视频999| 美女999久久久精品视频 | 久久久精品国产一区二区| 国产精品国产一区二区| 欧美精品www| 欧美一级片中文字幕| 免费在线观看亚洲视频| 免费看欧美一级片| 国产精品一区二区性色av| 国产精华一区| 欧洲精品久久久| 国产精品一区二区三区在线| 日韩在线观看免费高清| 亚洲www视频| 国产资源在线免费观看| 久久99国产精品99久久| 一区二区三区四区欧美日韩| 欧美日韩亚洲免费| 国产对白在线播放| 在线观看免费91| 麻豆成人av| 久久精品视频一| 天堂а√在线中文在线| 国产伦理一区二区三区| 国产精品久久久久久一区二区| 日韩欧美一区二区视频在线播放| 99在线观看视频网站| 超碰91人人草人人干| 欧美国产一二三区| 九色91视频| 欧美一区2区三区4区公司二百| 成人av免费电影| 欧美激情一区二区三级高清视频| 国内伊人久久久久久网站视频| www.欧美三级电影.com| 日本一区二区三区在线视频| 91九色对白| 中文字幕人妻熟女人妻洋洋 | 国产精品乱码| 欧美日本韩国在线| 九一国产精品视频| 日本精品一区二区三区在线播放视频| 91精品国产91久久久久久| 亚洲在线视频福利| 成人av影视在线| 一区二区精品视频| 99热在线这里只有精品| 一级特黄妇女高潮| 波多野结衣精品久久| 亚洲综合在线小说| 成人91免费视频| 亚洲一区二区三区四区视频| 99在线观看视频网站|