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WXR-700/2100Operational
Overview767
andClassic
737WXR-700(FLW
or
non-FLW)737ngMultiscanWXR-2100通过控制板鉴别飞机安装的Boeing系统通过控制板鉴别飞机安装的Boeing系统通过控制板鉴别飞机安装的Airbus系统AGENDAMultiScanTM
OverviewAviation
WeatherHow
Radar
WorksAutomatic
OperationManual
OperationMultiScanTM
Overview传统的使用及俯仰调节的作用As
the
radar
beam
moves
higher
in
the
thunderstormreflectivity
decreases结论:观察雷雨一定要观察雷雨的下部(根部),扫描雷雨的中上部位会造成回波弱的现象;但为了避免扫到过多的地面杂波影响对雷雨的观察,需要上调到一个折衷的俯仰角:既要观察雷雨的下部,又要避免产生过多的地面杂波,多波束
提供了解决方案能探测到的雷雨顶部实际雷雨高度
FREEZING
LEVEL纯雨量探测(绿黄红体现雨量的递增),增益需人工按需(例如气象环境)补偿需要俯仰调节,寻找雷雨反射体,同时要避免地面杂波Optimum
Tilt
for
Clutter
Rejection
OverScans
Significant
Weather
Except
inthe
50
-
80
nm
RangeOptimumTilt
for
Weather
DetectionProduces
Significant
Ground
Clutter3Down3Up2Up`1
Up0Degrees1Down2DownBest
WxDetectionBest
ClutterRejection传统的探测及使用特点多扫描自动模式的工作原理及特点1.充分利用波束逐渐变宽的特性,通过自动高低两个扫描即捕获取全程320nm气象信息2.( 器)融合数字化3.使用波束与波束的反射对比计算雷雨高度,并采用地形数据库进行地面杂波抑制两个波束的俯仰角由系统根据飞机的高度和地形自动设置,从而最佳的扫描雷雨的中下部(强反射率部位),起飞时两个波束向上看(上波束5.7度,下波束之高4.3度,显示为5度),随着飞机高度的增加,两个波束逐渐下俯,显示器上显示的为两个波束俯仰角的平均值.4.通过自动增益补偿,全球气象模型数据库,飞越保护对影响航路的
气象进行全面整体的体现(只显胁飞行高度的
气象)MultiScan
Operational
Capabilities40NM40
NM100
NMGround
Clutter
Free300
NM300
NMAttenuation
Alert40
NM
TurbulenceOverFlight
Protection200
NM200
NMGround
Clutter
Free
DisplayAttenuation
AlertCertified
Turbulence
to
40NMOverFlightTM
ProtectionPredictive
Windshear100
NM所有的气象情况都在 器里面,只显示影响飞行航路的雷雨Accurate
Weather
that
affects
the
aircraft
flight
path
from
thenose
of
the
aircraft
to
320
NM1st
Generation
Hazard ysis
based
onregion
and
timeof
year自动增益(对气象零温度线以上的部分进行的自动温度增益补偿)Temperature
Based
Gain(基于温度的增益补偿相当与增加了雷雨的反射顶,使能够看到雷雨更高的部分)MultiScan
increases
gain
automatically
above
freezing
level
with
A/C
altitude
increase
andoutside
temperature
decrease零温度线以上的自动温度增益补偿相当于增加了雷雨的可视高度HazardRainfallGreatestRainfallAircraft
flies
from
NorthAfrica
to
South
America.Hazard
over
SouthAmerica
is
relatively
mild南美气象 较低Cell
paints
green
overNorth
Africadue
tominimal
rainfall
rates.北非雨量很低Hazard
over
NorthAfrica
issevere北非气象TRRM
Sa lite
Data
–
Rainfall
RatesGreatest
rainfall
rate
isover
South
America.Storm
paints
red.南美雨量很大TRRM
Sa lite
Data
–
Reflectivity
at
30,000ft.全球气象模型数据库
(基于气象领域已建立的成
气象模型)根据飞机所在的位置,季节对照全球气象模型数据库,自动补偿增益,体现雷雨的真实
性根据飞机所在的位置,季节对照全球气象模型数据库,自动补偿增益,体现雷雨的真实
性Thunderstorm
Reflectivity
Characteristics
Vary
Dramatically
Depending
on
Season全球气象模型数据库
(基于气象领域已建立的成
气象模型)雷雨的湿顶到实际顶部的高度是与地域相关的,不同地域的气候条件会造成雷雨的发展高度有很大的不同,全球气象模型数据库根据大量的统计数据,建立了个全球各地域的气象模型,其中包括区域雷雨的发展高度(从湿顶向上的高度),会据此判断雷雨的实际高度,以确定是否对飞机高度具有性,从而显示只对飞行航路的气象气象学科的研究需要采用统计学,进行大量数理统计,建立成区域季节气象模型Multiscan
只是显飞行航路的雷雨胁与波音的Dark,Quiet
Cockpit概念相符全球气象模型数据库
(基于气象领域已建立的成
气象模型)全球气象模型数据库的补偿Gain
automatically
compensate
for
weather
variations
caused
by
varying
geographic
andclimatic
conditions.(雷雨的含水反射率随地域及季节会产生很大的变化,含水反射率不能体现雷雨的
,如对流活动及闪电)The
result
is
the
and
Only
Radar
that
provides
world
wide
hazarddetection.Captain's
Window Officer’s
WindowMultiScanLow
ReflectivityOceanic
WeatherGulf
of
Thailand湾区域的低反射气象图象依此为传统人工模式,人工最大增益模式及自动模式自动模式在低发射率的区域环境下会自动调高机器灵敏度,能看到传统 所无法体现的气象的整体情况Automatic
Gain
inAutoAUTOCAL
Gain
Gain
alsoadjusted
upon
the
geographical
regionMANUALCAL
GainMANUALMAX
GainOutsideForwardRight自动与人工模式3o
i1o
i0o2o
h3o
hMultiScanTM
AutomaticOperation2o
iBestWxDetection1o
hBest
ClutterRejectionMultiScanTM(GCS
Switch)Automatic
Operation.
Ground
Clutter
Suppression
turn
off.
This
is
the
picture
the
radar
is
actually
seeing.Automatic
Operation.
GroundClutter
Suppression
turn
on.Optimal
weather
return
on
all
rangescales.地面杂波的显示是很好的确认 工作性能的方法Aviation
Weather航空气象ReflectivityWet
HailDry
SnowRainDry
Hail提示:AirborneRadar
isDesigned
todetect
rain依靠探测雷雨中含水(降雨)量的多少来工作的,回波与雨量成正比;
无法
探测雪,雾,含水率低的云,干性湍流,闪电,区分冰雹与降雨的差别What
RADAR
Can’t
DoRadar
can’t
see
fog,
cloudwith
less
moisture,
snow,ice
crystalsRadar
can’t
see
lightning,clear
turbulenceRadar
can’t lthedifference
between
wethails
and
heavy
rainfall探测局限性系统是机组绕飞雷雨的辅助工具目前工业界采用的三种颜色级别显示无法定量的提示无法直接探测闪电的活动人工模式或传统 为单纯的雨量探测自动模式通象模型数据库建立雨量与(对流,闪电)在不同地域及季节的对应关系,通过颜色的补偿会提高对气象的提示雷雨的湿顶与目视顶Ice
Only
(Glaciated)7000
m
/25,000
ftMixed
iceand
waterFreezing
LevelLiquid
water
onlyRadar
topWarning!!
Significant
verticalthunderstorm
developmentwith
severe
turbulence
anddry
hail
may
exist
above
theradar
top.由于雷雨不同部分反射率的差异,会造成传统 在高空飞行回波弱的感觉,低空回波强的感觉,Multiscan在自动模式下会根据气象模型数据尤其在雷雨距离飞机较近的情况下(40海里以内),波束较细,未能进行较佳的俯仰调节 库判断雷雨的实际
顶部,体现 气象Single
Cell
Thunderstorm
Development1.
Warm,
humid
airrises
from
theground
in
thermalupdrafts.Towering
CumulusStageMature
Stage4.
When
ice
crystals
are
water
droplets
grow
big
enoughto
ethe
updraft
they
begin
to
fall
and
dragdown
the
surrounding
air.The
icecrystals
meltas
theydescend.The
fallingprecipitation
and
airbeing
dragged
downform
down
drafts.Existence
ofbothupdrafts
and
downdrafts
create
severturbulence.3.
Updraftscontinuefeeding
warm,humid
air
intothe
storm.Existence
ofboth
updraftsand
downdrafts
createseverturbulence.2.
As
the
air
cools
to
thedew
point,
the
watervapor
condenses
intoclouds.7.
Downdraftsgrow,
chokingoff
updrafts.8.
With
thesupply
ofhumid
air
cutthe
stormbegins
dyingand
the
raindecreases.DissipatingStageNote:
The
total
life
cycleshown
here
takes
approx-ima y
one
hour.1. Thunderstorm
development
is
rapid.Develo thunderstorms
cangrow
at
6,000’
per
minute.A
course
that
appears
clear
may
contain
cellsa
few
minutes
later.
成长上升过程20-30米/秒雷雨的不同发展阶段具有不同的 特性Newly
develo cells
often
do
not
contain
sufficient
water
to
reflect
an
echo,
yetthey
can
cause
severe
turbulence
or
lightning.3. Studies
haveshown
that
thunderstorms
tend
travel
in
the
direction
of
thewinds
around
10,000
feet.
New
cells
generally
formon
the
side
of
acloud
in
the
direction
towardwhichit
is
moving.雷雨的运动方向受10000英尺中高度风的影响雷雨的动态性Steady-state
ThunderstormsThunderstorm
may
be
5to10
meterStratosphere
40,000-60,000’4.
Overshoot3.
Gust
front2.
Mid
levelwinds1.
Warm,
moist
air5.
Upperlevel
winds6.
Anvil
topNote:
Steady-statethunderstorms
may
lastseven
to
eight
hours工作原理及基本概念系统Key
ElementsReceiver/TransmitterAntennaRadomeControl
PanelDisplayPeripheralsIRS/ADC/LRA/Discretes天线俯仰角The
3.5º
beamscans
+/-90ºaircraft
heading
and
takes
a“Slice”
out
of
theradar.Tilt
Angles
refers
toangles
between
centerline
of
beam
andhorizontal
planeManual
Tilt
Control
+/-15
degree
with
¼
increment
or
¼
incrementbetween
+/-5
degree
and
½
beyond
+/-0.5degreeThis
ti isplay
is
driven
by
the
Arinc
453
dataword
from
the
WRT.The
WRT
gets
this
information
from
controlsource/WCP
providing
the
Tilt
commandThe
WR
d
a
tilt
command
to
theAntenna,The
antenna
tilts,
the
WRT
see's
the
feedbackand
everything
is
OK.
if
not
then
the
WRT
setsthe
ANT
fault
message.If
OK
then
set
display
data
on
the
Arinc453Data
bus,
and
displaysTilt
value
on
ND.The
system
spec
for
this
is
less
then
2
degreesdifference
between
the
Control
Panel
and
thedisplayed
value.天线稳定性(Stabilization)RadarScansparallel
to
theHorizonStabilizationOnRadar
Scansparallel
to
theaircraft’s
wingsStabilization
OffNon
multiscan
radar
control
panelSTAB
need
to
be
ON
all
the
time,STAB
shows
if
selected
OFFCOLOR
SCHEMEBlack:
Less
Than
.76
mm/hr(.03
in/hr)Green:
Weak
(20
dBz).76
-
3.81
mm/hr
(.03-.15in/hr)Yellow:
Moderate
(30
dBz)3.81-12.7
mm/hr
(.15-.5
in/hr)Red:
Strong
to
Very
Strong12.7(40
dBz
and
Greater)mm/hr
(.5
in/hr)
and
GreaterMagenta:
Turbulence(Greaterthan
5
meters/second
wind
velocity)增益及校准增益Calibrated
Gain人工模式CAL=降雨反射率自动模式CAL=降雨反射率+基于温度的自动补偿+全球气象模型数据库的补偿注:人工模式
通过颜色级别来显示雷雨的强弱,但颜色的等级与闪电的活动和气流的强烈并无正比关系,很多情况,绿色(新形成的雷雨)可能会伴随着频繁的闪电活动和气流(颠簸)的运动。CAL增益下雷雨强度与颜色级别的对比关系Gain
Controls(Multiscan
Controls)6CAL
GainPositionGain
Control
Settings(Manual
Operation)AirbusBoeingEffects
of
Gain
SelectionCalibrated
Gain+8+16+4-2-4-6-8-12-14亮带(负增益的使用)Bright
Band(Bright
Band/RedOut)全红现象全红产生的两个原因大面积强降雨包含大尺寸的雨滴大面积层云零温度线下产生亮带层次(雪包着水),亮带以下可能只为轻雨或小雨(飞机下降至亮带以下, 波束如离开亮带,全红的现象可能
)Bright
Band
occurs
at
and
below
thefreezing
level
in
strata
form
cloudformations.Cockpit
DisplayBright
Band波束特性Beam
CharacteristicThe
3.5
degree
beamtakes
a
“Slice”
out
of
theradar
.Beam
Characteristics(Beam
Diameter)Approximate
Beam
Width
Formula:Beam
Width
(in
feet)
=
(Distance
in
Nm
+
“00”)
x3.5Beam
Width
(50
Nm)
=
17,500
ft300
Nm105,000
ft200
Nm70,000
ft100
Nm35,000
ft50
Nm17,500
ft10
Nm3,500
ft距飞机越近,波束越窄,扫到雷雨的切面越薄, 的信息点越多,显示雷雨的分辨率越好距飞机越远,波束越宽,更容易扫到雷雨,但雷雨的分辨率差发出的波束为3.5发散角的圆锥体Beam
Characteristics(Range
and
Azimuth
Resolution)AzimuthResolution(due
to
beam
width)RangeResolution(dueto
pulse
width)Beam
CharacteristicsSummaryThe
best
weather
definition
occurswithin
80
NMof
the
aircraft.
Beyond80
NM,
the
radar
should
be
used
forflight
path
planning
purposes,
not
forweather
ysis.结论距离越远,波束越宽,
分辨雷雨细节的能力越差建议80nm以内对目标进行分析80nm以外的显示主要作为确认目标的位置与存在及进行飞行计划Beam
Characteristics
&
Attenuation随着飞机与雷雨的相对靠近,由于波束变细和波束能量距离传递损耗的减少,雷雨的细节更清楚,尺寸有所增长,绿色增加是正常现象STC的有限调节能力(40海里以内)TimeReceiver
Sensitivity随着飞机接近云间通道,波束能量衰减减少,绿色可能逐渐充溢通道(自动模式)Beam
Characteristics
&
AttenuationPath
Attenuation(Radar
Shadow)Note
steep
gradient
andconcave
shape
on
back
ofstormAim
radar
beam
towardsthe
groundIf
ground
clutter
appearsat
the
sides
of
the
stormbut
not
behind
it,
this
is
aradar
shadow.
The
areabehind
the
stormisattenuated.Note:
Mountains
alsoproduce
radar
shadows.Never,
Never,
Ever
Fly
Into
aRadar
ShadowArea
of
possiblesevere
attenuationPATHATTENUATIONCompensation
and
AlertPAC
AlertCompensates
ForAttenuation
Due
ToInterveningPrecipitation
(UpTo
Approxima
y80nmi)WhenCompensationLimitReached,Alert
AnnunciatesAreas
whereSevere
Attenuationis
Occurring
(PACAlert
Bar)PAC
Alert
Unique
toCollins
RadarPAC
Alert
Bar
Warns
Crew
ofSevere
AttenuationNoteCalibrated(CAL)Gain
must
beselected
for
thePAC
Alert
tofunctionPath
Attenuation(Southern
Airways
Flight
242,DC-9)Pilot’s
Radar
PresentationActualWeatherSince
1975
at
LeastTen
Fatal
Accidents
Have
Occurred
in
the
United
StatesWhere
Radar
Attenuation
was
a
Major
Contributing
FactorAircraft
Penetrates
ExtremeThunderstormReaching
to
55,000Feet
that
is
Producing
Tornadoesand
Three
Inch
HailAttenuation
SequenceForward
LookingWindshearMicrobursts
&
WindshearMETERSApproachFlight
Path40
KnotHeadwind40KnotTailwindAIRSPEEDPOWER0200
0ALTITUDEApproach
andGo
AroundTakeOff3
nm0.25nm0.25nm3030Windshear(Detection
Zones
–
Airbus
and
retrofitaircraft)0.25nm0.25nmWarningCautionAdvisoryWeather
Detection
Region5
nm3
nm30305
nmWindshear(Detection
Zones
–
Boeing
aircraft)Approach
andGo
AroundTake
Off3
nm0.25
nm0.25nm30300.25nm0.25nmWarningCautionWeather
Detection
Region5
nm3
nm30305
nm2,300’1,200’
-
50’2,300’0Kts
-1,200’Windshear(Vertical
Alert
Zone)TakeoffLanding100
Kts
-
50
FT50
-
0
FTPWS
Fail
only
occurbelow
2300’PWS
Auto
Turn
On
Throttle
SW53
Degree
Advance(Boeing737ng)No2/No3
Engine
above
idle(takeoff
thrust/B747)Discrete
from
EIUOil
Pressure
and
GroundSpeed/30K(Airbus)Boeing
Failure
MessagesNOTE:
Write
Down
Failure
Messages
For
MaintenanceWXR
ATT:
Attitude
input
failsWXR
STAB:
Stabilization
is
off.No
AUTOTILT(自动模式失效,可选择人工模式使用)WXR
FAIL(lossof
Image)R/TWXR
control
panelWXRantennaPWS
failure:Loss
ofanyRA
*
Lossof
ADR
dataLoss
of
IR
data
*
antenna
faultsInternal
WXRsystem
faultsLoss
of
CAS
and
TAS.注: 有严格的 电路,如反射功率等的降低到一定门限,会触发WXRFAIL,说明 失效,一般情况下,不要轻易认为 回波弱,功率不够Failures(loss
of
the
radar
image)are
displayed
in
redWXR
R/T
:
failureR/TWXR
ANT:
failure
of
antennaWXR
CTL:
failure
of
CTLWXR
RNG:
comparison
errorbetween
therange
from
the
EFIS
section
and
thecopydata
received
on
the
DMC
via
theradardata
busFailures
(image
not
loss/amber)PRED
W/S
:
windshear
function
failureWXR
ATT:
ADIRU
attitude
failureNO
AUTOTILT:(自动模式失效,可选择人工模式使用)WXR
STAB:loss
of
the
radar
antenna
stabilization(deselect
STAB
from
CP)WXR
TEST
:
TEST
modeAirbus
Failure
MessagesNOTE:
Write
Down
Failure
Messages
For
MaintenancePWS
Fail
on
AirbusNOTE:
Write
Down
Failure
Messages
For
MaintenanceExternal
Triggers
of
PWS
FailExternal
FaultTime
To
SetTime
To
ResetNote:Radio
Altimeter4s2
valid
words/sin
4sAirspeed12s0Heading12s1
valid
word/SIn
12sAttitude
Input,Pitch/Roll(Left
ADIRUusednormally)12s4sAlso
trigger
ATTmessageAir/Gnd
vs.
Rad
AltAir
RA
<
20
ft.
for
>
30
secON
Gnd
and
RA
≥
20ftfor
10sec0Pitch/Roll
vs.
Air/GndOn
Ground,
Pitch
>
7and/or
Roll
>5
deg.
thenset
in
20sec.NOAUTOTILT自动模式失效,可选择人工模式使用NO
AUTOTILT:
Loss
Data
From
ADIRU(for12s)Only
displayed
when
AUTO
modeselectedAirspeedHeadingBarometric
AltitudeSATDrift,
Track
AngleGround
SpeedLON/LATRadome
CharacteristicsThe
Radome
is
your
radar’swindow
to
the
outside
world.If
the
“window”
is
dirty
ordamaged,
radar
energy
willnot
shine
through
clearly.Radome
ClassesDO-213
references
the
percentage
ofRF
energy
that
can
pass
through
theradome
as
Transmission
Efficiency(Transmissivity):AverageMinimum
at
any
PointClass
A90%85%Class
B87%82%Class
C84%78%Class
D80%75%Class
E70%55%Radome
Characteristics(Cat’s
Eyes)Cat’s
Eyes“Cats’
Eyes”
or
“Ghost s”
mayappear
in
a
narrow
greenor
greenyellow
arcor
as
twosmall s
at
+/-45
Degrees,
between
the
4
and
8ranges
and
the
aircraft
altitude
is
aboveapproxima y
3,000
ft.
This
representsside
lobe
reflections
fromthe
groundand
is
caused
by
either
turning
the
gaintowardsthe
max
position
or
by
aRadome
with
greatly
reducedtransmitivity.SafetyBoeing:
50
FT
(15
M)
FROM
THE
RADAR.Airbus,
more
than
5
meters
(16.4FT)
from
the
antenna.No is
in
the
area
made
by
an
arc
of
135
degree
on
eachside
of
A/Ccenterline.The
greatest
radiated
power
density(1.43mW/cm2,18
inches
fromantenna)
of
theCollins
WXR-2100
WeatherRadar
System
issignificantlylessthan
the
10
mW/cm2
allowable
for
limiting
the
exposure
of
rf
energyto
humans
as
noted
in
FAA
Advisory
Circular,
number
20-688,
datedAugust
1980.AlienRadarMultiScanTMAutomatic
OperationControl
PanelsBoeingAirbusDisplay
Annunciations(Airbus)Display
Annunciations(Boeing)Tilt
Annunciation(What
Does
it
Mean?)Controls(PowerOn/Off)AirbusOnlyNote:
On
Boeing
aircraft,
power
isapplied
to
the
radarsystem
byselecting
“WXR”
on
the
EFIS
control
panel.Controls(Automatic
Operation
(On/Off))Automatic
Operation
InitializationManualSweepSecondSweepThirdSweepFourthSweepFifthSweep1,当选择自动模式时,
需要进行4个扫描起始过程
2,在正常自动模式的工作状态下,如在短时间内选择人工方式(38秒内),再转回自动模式,因为
了先前的自动设置,所以不需再进行起始过程.对安装双套
系统的情况,由原正常工作的系统转化至另套系统也需经过起始显
示地面杂波的过程自动模式的自动调节补偿,抑制地面杂波Auto
Alignment
Process现象:自动模式爬升或巡航阶段观察到地面杂波(一般在80海里左右或以外),原因:在更换
R/T或 驱动器之后,
需在第一次飞行的巡航高度,自动调整以补偿系统安装误差及飞机在空中结构弯曲变化造成对零参考面的影响,以实现高精度的波束俯仰角度,用以计算地面杂波的滤除.调整过程中杂波的出现并不影响中近程雷雨的探测,同时也可按需使用人工方式调整过程的实现需要在飞机进入平飞状态,巡航高度,陆地飞行的情况下进行,一般需要几分钟的时间.调整结束后地面杂波完全滤除,此种情况下
的工作完全正常.Auto
Mode
Ground
Clutter
Suppression
RequiresPrecise
Knowledge
of
Radar
Antenna
Position杂波抑制需知道天线波束的精确俯仰角度Antenna
Drive,
IRS
Installation
Variations天线驱动器和惯导系统的安装差异Aircraft
Flex
in
Flight
(transition
from
groundstatic
calibration)飞机结构在空中的柔性变化对零参考线的影响Auto
Alignment
Process
in
cruise
will
compensatefor
these
variations在巡航平飞开始后会进行自我调整(几分钟),补偿上述误差,杂波的出现并不影响中近程雷雨的探测,同时也可使用人工进行确认Controls(Dual
System
Selection)Controls(PWS
(Predictive
Windshear))Airbus
OnlyGain
Controls(Controls)6CAL
GainPositionGain(Operating
Techniques)CAL
Gain
is
the
mendedoperating
positionStandard
Color
LevelsPAC
AlertFunctionCaution:
Always
return
gain
to
CAL
aftera
below
CAL
gain
setting
has
been
utilized.
BelowCAL
gain
settings
may
cause
thunderstorms
to
appear
less
intense
than
is
actually
the
case.Caution:PAC
Alert
(attenuation/radar
shadow)
is
disabled
for
all
non-CAL
settings.Controls(Tilt
Control)ControlsGround
Clutter
(On/Off)ControlsWX
(Weather
Mode)ControlsWX+T
(Weather
Plus
Turbulence
Mode)On
All
RangeScalesOutto40
nmControlsTURB
(TurbulenceMode)Airbus
OnlyCaution:
Precipitation
will
not
be
displayed
when
operating
in
TURBmode.Inadvertentpenetration
ofareas
of
severe
weather
is
possible.Controls(MAPmode)Interstate
90Interstate
88Interstate
55Interstate
80LakeMichiganControlsTFR
(Transfer)Boeing
OnlyNote:
If
both
pilots
select
TFR
(transfer)the
radar
will
be
unable
to
determinewhich
setting
to
use
and
a
TEST
patternwill
be
displayed
on
the
EFIS.Controls(TEST)BoeingOnlyNote:
On
Airbus
aircraftactivated
throughthe
CFDS.
Step
by
stepinstructions
are
provided.Select
a
non-TEST
modeon
theradar
control
panelSelect
WXR
on
the
EFIScontrolpanelPress
TESTAutomatic
Features(Optimized
Weather)10
nm20
nm40
nm320
nm160
nm80
nm0-320
nmWxOver-ScanningProblem:How
do
you
preventover
scanning
andinadvertent
thunder-storm
top
penetrations?80%
Below
25,000’It
is
difficultto
AvoidOver
Scanning
Top
ofcells
at
or
just
belowthe
aircraft
altitude.Industry
DiscussionsSuggest
that
much
ofwhat
we
call
CAT,
isreally
turbulenceassociated
with
weather
at
or
just
below1st
the
aircraft
altitude:65%
Above
25,000’1st80nm3rd3rd20
nm2nd2nd40
nmThe
contents
ofthisare
proprietaryto,
Inc.84OverFlightTM
Protection10
NM30
NM25
NM20
NM飞跃保护在22000ft启动会
低于飞行高度约6000ft的雷雨(雷雨反射体的顶部与飞机的相对高度),并始终保持在显示器上132213Storms
at
60,
100and
180NM
visible
on
theradar
display
and
verifiedfromthecockpitTurbulence
indicated
out
to
40
NMPAC
Alert
barLong
Range
WeatherDetection(0
-
320
NM
Weather,
Turbulence
and
PAC
Alert
on
a
single
display!!)Automatic
Features(Windshear
Alerts)Approach
and
Go-Around
Alert
RegionAreas
of
Windshear
When
Aircraft
in
AirWARNICAUTIOADVISONG
N
RY0.25nm30305
nm3
nm0.25nmQuiet,
Dark
Cockpit
–
Low
Level
Weather
EliminationFlight
Example
fromMIT-Lincoln
Labs
Flight
Aug
17,
2008Low
Level
Non-ThreatWeather
is
Stored
inComputer
Memory,butnot
Displayed自动模式只显 胁飞行航路的雷雨,避免不必要的干扰建议由巡航转入下降前从自动转化至人工模式调低天线角度,观察低空雷雨的情况随着飞机的逐步下降,再转回自动模式Update
Rates(AUTO)The
antenna
scan
is
nolonger
tied
to
thedisplaysweep.
Sweep
line
issimulated.MultiScan
updates
all
radardisplays
every
four
secondsin
allmodes
exceptwindshear,
in
which
case
thedisplays
update
every5.5secondsAutomatic
Features(Simultaneous
Display
Updates
in
All
Range/ModeCombinations)Captain
and Officer’s
displays
simultaneously
updated
every4
seconds
in
all
modes
except
windshear.Captain
and Officer’s
displays
simultaneously
updated
every5.5
seconds
during
windshear
operation.Only
shows
the
simulated
sweep
line
from
left
to
right.
Thesimulated
sweep
line
may
not
synchronize
with
radar
beam
likethe
traditional
radarMultiScanTMManual
OperationControls(Manual
Operation
–
On/Off)如对自动模式有疑问,人工模式可随时选择,人为的控制俯仰,搜索雷雨的反射体Controls(Ground
Clutter–
Inactive
During
Manual
Operation)Inactive
duringmanual
operationControls(Tilt
Control)Tilt
control
is
THE
mostimportant
factor
forsuccessful
operationofthe
radar
duringmanualoperation.Too
HighToo
LowCompromiseTilt
Management(Optimum
Tilt
Angle)
FREEZING
LEVELOptimum
Tilt
for
ClutterRejection
Over
ScansSignificant
Weather
Except
inthe
50
-
80
nm
RangeOptimum
Tilt
for
WeatherDetectionProducesSignificant
Ground
ClutterBest
WxDetectionBest
ClutterRejectionCompromise
Tilt
AngleTilt
Management(LowAltitude
Tilt
Settings
–
10,000’
and
Below)LowAltitudeTiltControlTilt
=
+2.0
to+7.0mended
10,000
feetand
belowTilt
Management(Low
Altitude
Tilt
Settings
-
Take
Off
/
Climb)Five
degrees
up
tilteliminates
clutterand
keeps
theradarbeam
pointedgenerally
along
theaircraft
flight
pathCaution:
If
the
tiltsetting
is
too
highthe
radar
mayscanover
the
opts
ofthreatthunderstorms.If
the
tiltsetting
is
toolow,
the
radar
may
failtodetect
vaultedthunderstorm
energy.3000
fpmrate
of
climb240
kts(24,304
fpm*)Note:
1
degree
of
tilt
gives
you
100
foot
per
nautical7oofbeam
position
change(e.g.
15
degrees
at
20=
30,000
feet)*Conversion
Factor:
6067
ft/NM3o5o15o7oTilt
Management(扫描地波毛边)(Mid
AltitudeTilt
Control
(10,000’-25,000’))Note:
The
clutter
ring
in
mountainous
areas
may
beless
well
defined
than
in
non-mountainousareasMiddle
Altitude
Tilt
Control(10,000’
to
25,000’)Adjust
tilt
sothatgroundclutter
is
displayed
attheedge
of
the
radar
displayto
minimizethepossibility
ofscanningoverthe
top
of
threatweather.80
and40
nmrangescalesCaution:
Below
25,000’
asmuch
as80%
of
clear
air
turbulenceencounters
are
weather
related
and
are
often
due
to
over-scanning.Clutter
RingClutter
Ring
inmountainousarea基于扫描地波毛边的俯仰设置理念,大幅调低天线,再慢慢调起Tilt
Management(扫描地波毛边)(Guidelines)80
nmAt
given
altitiude
and
range
scale,
with
enoughground
clutter
on
display,
slowly
tiltup
antenna
to
reduce
the
ground
return
totheextent
of
small
layer
on
the
outer
edge
ofdisplay.
Sometimes,
a
plus
tilt
setting
might
berequired
to
achieve
this.Tilt
Management探测的死角(雷雨与飞行高度接近)Tilt
Management(扫描地波毛边)(Guidelines)不同距离圈设置的扫毛边图示Tilt
Management(Mid
AltitudeTilt
Control
(10,000’-25,000’))160
nmRange
ScaleCaution:
Below
25,000’
asmuch
as80%
of
clear
air
turbulenceencounters
are
weather
related
and
are
often
due
to
over-scanning.Radio
HorizonTiltManagement(High
Altitude
Tilt
Control
(25,000’
andAbove)High
AltitudeTilt
Control(25,000
feetand
above)Adjust
tilt
so
thatgroundclutter
is
displayed
attheedge
of
the
radardisplayto
minimize
thepossibility
of
scanningoverthe
top
of
threatweather.Warning:
Over-scanning
and
subsequent
inadvertent
thunder-storm
top
penetration
is
a
significant
threat
above25,000’.Over-ScanningProblem:How
do
you
prevent
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