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 >

時間:2011-02-04 12:07來源:藍(lán)天飛行翻譯 作者:admin
曝光臺 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

altimeter for accuracy before every flight. To check and set the altimeter:
3.11.6.1. Set the current altimeter setting on the barometric scale.
3.11.6.2. Check altimeter at a known elevation and note the error in feet.
3.11.6.3. Set the reported altimeter setting on the barometric scale and compare the indicated altitude to
the elevation of a known checkpoint.
AFPAM11-216 1 MARCH 2001 101
3.12. Nonstandard Atmospheric Effects. The altimeter setting is a correction for nonstandard surface
pressure only. Atmospheric pressure is measured at each station and the value obtained is corrected to
sea level according to the surveyed field elevation. Thus, the altimeter setting is the computed sea level
pressure and should be considered valid only in close proximity to the station and the surface. It does not
reflect nonstandard temperature nor distortion of atmospheric pressure at higher altitudes.
3.13. Types of Altitude:
3.13.1. Indicated Altitude. This is the value of altitude that is displayed on the pressure altimeter.
3.13.2. Calibrated Altitude. Calibrated altitude is indicated altitude corrected for installation or position
error.
3.13.3. Pressure Altitude (PA). The height above the standard datum plane (29.92" Hg and 15 oC) is
PA (Figure 3.13.)
3.13.4. Density Altitude (DA). Density is mass per unit volume. The density of the air varies with
temperature and with height. Warm air expands and is less dense than cold air. Normally, the higher the
PA, the less dense the air becomes. The density of the air can be expressed in terms of the standard
atmosphere. DA is the PA corrected for temperature in the density altitude window of the dead
reckoning (DR) computer. This calculation converts the density of the air to the standard atmospheric
altitude having the same density. DA is used in performance data and true airspeed (TAS) calculations.
3.13.5. True Altitude (TA). TA is the actual vertical distance above mean sea level (MSL), measured in
feet. It can be determined by two methods:
3.13.5.1. Set the local altimeter setting on the barometric scale of the pressure altimeter to obtain the
indicated true altitude (ITA). The ITA can then be resolved to TA by use of the DR computer (Figure
3.17).
3.13.5.2. Measure altitude over water with an absolute altimeter.
3.13.6. Absolute Altitude. The height above the terrain is called absolute altitude. It is computed by
subtracting terrain elevation from TA, or it can be read directly from a radar altimeter.
3.14. Computer Altitude Solutions. The two altitudes most commonly accomplished on the computer
are TA and DA. Nearly all DR computers have a window by which DA can be determined; however, be
certain that the window is labeled density altitude.
3.14.1. True Altitude (TA) Determination. In the space marked FOR ALTITUDE COMPUTATIONS
are two scales: (1) a centigrade scale in the window and (2) a pressure altitude (PA) scale on the upper
disk. When a PA is placed opposite the temperature at that height, all values on the outer (miles) scale
are equal to the corresponding values on the inner (minutes) scale increased or decreased by 2 percent
for each 5.5 oC that the actual temperature differs from the standard temperature at that PA, as set in the
window. Although the PA is set in the window, the ITA is used on the inner (minutes) scale for finding
the TA, corrected for difference in temperature lapse rate.
102 AFPAM11-216 1 MARCH 2001
EXAMPLE:
Given: PA 8,500 feet
Given: ITA 8,000 feet
Given: Air Temperature –16 oC
To Find: TA
Procedure: Place PA (8,500 feet) opposite the temperature (-16) on the FOR ALTITUDE
COMPUTATIONS scale. Opposite the ITA (8,000 feet) on the inner scale, read the TA (7,600 feet) on
the outer scale. The solution is illustrated in Figure 3.l7.
Figure 3.17. Finding True Altitude.
3.14.2. Density Altitude (DA) Determination. DA determination on the computer is accomplished by
using the window just above FOR AIRSPEED AND DENSITY ALTITUDE COMPUTATIONS and the
small window just above that marked DENSITY ALTITUDE.
EXAMPLE:
Given: PA 9,000 feet
Given: Air temperature 10o C
To Find: DA
Procedure: Place pressure altitude (9,000 feet) opposite air temperature (10) in window marked FOR
AIRSPEED AND DENSITY ALTITUDE, read DA (10,400 feet). The solution is illustrated in Figure
3.18.
Figure 3.18. Finding Density Altitude.
AFPAM11-216 1 MARCH 2001 103
Section 3E— Absolute Altimeter
3.15. Basics. Accurate absolute altitude is an important requisite for navigation, airdrop, and bombing as
well as for safe aviating. It is particularly important in pressure pattern navigation. Absolute altitude may
be computed from the PA readings if the position of the aircraft is known, but the results are often
 
中國航空網(wǎng) www.k6050.com
航空翻譯 www.aviation.cn
本文鏈接地址:F16 Flying Operations AIR NAVIGATION(53)
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
成人国产精品一区| www欧美日韩| 国产福利不卡| 亚洲一区二区三区午夜| 国产自偷自偷免费一区| 久久精品国产精品国产精品污| 亚洲一区二区精品在线观看| 粉嫩av免费一区二区三区| 欧美乱人伦中文字幕在线| 免费特级黄色片| 国产精品视频午夜| 人妻无码久久一区二区三区免费| 久久久视频免费观看| 一区二区三区国| 国产伦精品一区二区三区精品视频| 国产精品人人做人人爽| 白白操在线视频| 欧美理论片在线观看| 红桃av在线播放| 欧美一乱一性一交一视频| 国内外免费激情视频| 日韩中文字幕在线免费观看| 日本va中文字幕| 久久久久久久激情视频| 91精品天堂| 亚洲第一页在线视频| av天堂永久资源网| 自拍视频一区二区三区| 99久re热视频这里只有精品6| 国产一区二区三区黄| 插插插亚洲综合网| 国产美女作爱全过程免费视频| 久久97久久97精品免视看| 国产美女久久精品| 中文字幕日韩精品久久| 91精品久久久久久久久青青| 在线观看一区欧美| 91国产在线免费观看| 日韩av不卡在线播放| 久久观看最新视频| 男人天堂a在线| 久久中文字幕在线视频| 国产奶头好大揉着好爽视频| 亚洲一区中文字幕| 久久久久久香蕉| 精品人妻一区二区三区四区在线| 国产精品国产亚洲精品看不卡15| 国产日产欧美a一级在线| 亚洲熟女乱色一区二区三区 | 国产成人精品一区| 国产专区一区二区三区| 亚洲一区二区精品在线| 久久精品一二三区| 免费一区二区三区| 亚洲免费在线精品一区| 日韩在线免费av| 国产三区精品| 日韩av色综合| 麻豆乱码国产一区二区三区| 91九色国产社区在线观看| 日韩久久久久久久| 精品免费国产| 国产成人一二三区| 国产一级片91| 天天综合中文字幕| 久久夜色撩人精品| 久久免费高清视频| 国产日韩中文字幕在线| 日韩福利在线| 久久久久国产精品一区| 日韩在线观看网址| av免费中文字幕| 黄色片视频在线免费观看| 亚洲a在线观看| 国产精品高清网站| 国产成人精品免费视频大全最热 | 亚洲www在线观看| 国产精品免费区二区三区观看| 亚洲 国产 欧美一区| 久久躁日日躁aaaaxxxx| 国产黑人绿帽在线第一区| 免费国产一区二区| 亚洲va欧美va在线观看| 国产精品成人免费视频| 日本精品性网站在线观看| 欧美激情一级二级| 国产精品入口福利| 国产成人精品久久| 91老司机精品视频| 久久久人成影片一区二区三区 | 久久99导航| 97免费高清电视剧观看| 国产中文字幕免费观看| 欧美在线www| 日本一区二区三区在线视频| 亚洲直播在线一区| 精品自在线视频| 国产精品久久久久久久9999| 久久久久亚洲精品| 久久免费高清视频| 99在线影院| 国产日韩在线精品av| 欧美一区二区影院| 日本欧美在线视频| 在线丝袜欧美日韩制服| 国产精品久久久久秋霞鲁丝| 久久精品国产99国产精品澳门| 国产高清免费在线| 99热一区二区三区| 国产精品专区一| 国产日韩中文字幕| 国产一区二区高清视频| 精品午夜一区二区| 国产在线视频一区| 国产一级片黄色| 国产欧美日韩综合一区在线观看| 精品亚洲第一| 国产亚洲第一区| 国产一区二区色| 欧美连裤袜在线视频| 欧洲成人在线观看| 欧美日韩国产高清视频| 欧美一级大片在线观看| 欧美少妇一区二区三区| 欧美精品七区| 麻豆传媒一区二区| 国模精品娜娜一二三区| 国模精品系列视频| 国产综合欧美在线看| 国产一区二区三区色淫影院 | 97久久精品视频| 超碰97网站| 国产精品亚洲激情| 成人免费91在线看| 8090成年在线看片午夜| 国产激情在线观看视频| 久久久久久久久久av| 国产精品视频久| 国产精品成人品| 欧美日韩高清在线观看| 亚洲一区二区三区在线免费观看| 春日野结衣av| 日本欧美黄网站| 青青草一区二区| 国产在线视频91| 成人h在线播放| 国产freexxxx性播放麻豆| www国产91| 毛片精品免费在线观看| 在线视频一二三区| 日韩亚洲在线视频| 国内自拍中文字幕| 国产美女搞久久| 77777亚洲午夜久久多人| 色婷婷综合久久久久| 国产精品福利小视频| 在线观看欧美一区| 日韩在线第一区| 欧美精品亚洲| 99久久激情视频| 日韩中文理论片| 久久99视频免费| 日韩中文字幕在线免费| 男人舔女人下面高潮视频| 国产精品一区二区三区不卡| 91成人福利在线| 国产精品日韩欧美一区二区| 一区二区三区三区在线| 日韩高清av| 国产日韩在线看| 国产精品com| 不卡毛片在线看| 日韩中文字幕在线不卡| 激情小说综合网| 91精品国产综合久久久久久丝袜| 久久视频这里只有精品| 亚洲综合中文字幕在线| 欧洲午夜精品久久久| www插插插无码免费视频网站| 久久久久久久少妇| 中文字幕99| 男人天堂新网址| 久久免费视频这里只有精品| 精品免费国产一区二区| 欧美中文字幕第一页| 成人免费网站在线| 国产精品视频免费在线观看| 午夜精品一区二区在线观看的| 欧美极品欧美精品欧美| 国产精品91在线| 国产999在线| 欧美精品一区在线| 久久久中文字幕| 欧美激情亚洲综合一区| 欧美精品一区三区在线观看| 久久婷婷人人澡人人喊人人爽| 久久久亚洲国产| 在线视频精品一区| 国产一区二区在线免费| 国产成人精品一区二区在线|