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WXR-700/2100Operational
Overview767
andClassic
737WXR-700(FLW
or
non-FLW)737ngMultiscanWXR-2100通過控制板鑒別飛機安裝的Boeing系統(tǒng)通過控制板鑒別飛機安裝的Boeing系統(tǒng)通過控制板鑒別飛機安裝的Airbus系統(tǒng)AGENDAMultiScanTM
OverviewAviation
WeatherHow
Radar
WorksAutomatic
OperationManual
OperationMultiScanTM
Overview傳統(tǒng)的使用及俯仰調(diào)節(jié)的作用As
the
radar
beam
moves
higher
in
the
thunderstormreflectivity
decreases結(jié)論:觀察雷雨一定要觀察雷雨的下部(根部),掃描雷雨的中上部位會造成回波弱的現(xiàn)象;但為了避免掃到過多的地面雜波影響對雷雨的觀察,需要上調(diào)到一個折衷的俯仰角:既要觀察雷雨的下部,又要避免產(chǎn)生過多的地面雜波,多波束
提供了解決方案能探測到的雷雨頂部實際雷雨高度
FREEZING
LEVEL純雨量探測(綠黃紅體現(xiàn)雨量的遞增),增益需人工按需(例如氣象環(huán)境)補償需要俯仰調(diào)節(jié),尋找雷雨反射體,同時要避免地面雜波Optimum
Tilt
for
Clutter
Rejection
OverScans
Significant
Weather
Except
inthe
50
-
80
nm
RangeOptimumTilt
for
Weather
DetectionProduces
Significant
Ground
Clutter3Down3Up2Up`1
Up0Degrees1Down2DownBest
WxDetectionBest
ClutterRejection傳統(tǒng)的探測及使用特點多掃描自動模式的工作原理及特點1.充分利用波束逐漸變寬的特性,通過自動高低兩個掃描即捕獲取全程320nm氣象信息2.( 器)融合數(shù)字化3.使用波束與波束的反射對比計算雷雨高度,并采用地形數(shù)據(jù)庫進行地面雜波抑制兩個波束的俯仰角由系統(tǒng)根據(jù)飛機的高度和地形自動設(shè)置,從而最佳的掃描雷雨的中下部(強反射率部位),起飛時兩個波束向上看(上波束5.7度,下波束之高4.3度,顯示為5度),隨著飛機高度的增加,兩個波束逐漸下俯,顯示器上顯示的為兩個波束俯仰角的平均值.4.通過自動增益補償,全球氣象模型數(shù)據(jù)庫,飛越保護對影響航路的
氣象進行全面整體的體現(xiàn)(只顯脅飛行高度的
氣象)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所有的氣象情況都在 器里面,只顯示影響飛行航路的雷雨Accurate
Weather
that
affects
the
aircraft
flight
path
from
thenose
of
the
aircraft
to
320
NM1st
Generation
Hazard ysis
based
onregion
and
timeof
year自動增益(對氣象零溫度線以上的部分進行的自動溫度增益補償)Temperature
Based
Gain(基于溫度的增益補償相當(dāng)與增加了雷雨的反射頂,使能夠看到雷雨更高的部分)MultiScan
increases
gain
automatically
above
freezing
level
with
A/C
altitude
increase
andoutside
temperature
decrease零溫度線以上的自動溫度增益補償相當(dāng)于增加了雷雨的可視高度HazardRainfallGreatestRainfallAircraft
flies
from
NorthAfrica
to
South
America.Hazard
over
SouthAmerica
is
relatively
mild南美氣象 較低Cell
paints
green
overNorth
Africadue
tominimal
rainfall
rates.北非雨量很低Hazard
over
NorthAfrica
issevere北非氣象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.全球氣象模型數(shù)據(jù)庫
(基于氣象領(lǐng)域已建立的成
氣象模型)根據(jù)飛機所在的位置,季節(jié)對照全球氣象模型數(shù)據(jù)庫,自動補償增益,體現(xiàn)雷雨的真實
性根據(jù)飛機所在的位置,季節(jié)對照全球氣象模型數(shù)據(jù)庫,自動補償增益,體現(xiàn)雷雨的真實
性Thunderstorm
Reflectivity
Characteristics
Vary
Dramatically
Depending
on
Season全球氣象模型數(shù)據(jù)庫
(基于氣象領(lǐng)域已建立的成
氣象模型)雷雨的濕頂?shù)綄嶋H頂部的高度是與地域相關(guān)的,不同地域的氣候條件會造成雷雨的發(fā)展高度有很大的不同,全球氣象模型數(shù)據(jù)庫根據(jù)大量的統(tǒng)計數(shù)據(jù),建立了個全球各地域的氣象模型,其中包括區(qū)域雷雨的發(fā)展高度(從濕頂向上的高度),會據(jù)此判斷雷雨的實際高度,以確定是否對飛機高度具有性,從而顯示只對飛行航路的氣象氣象學(xué)科的研究需要采用統(tǒng)計學(xué),進行大量數(shù)理統(tǒng)計,建立成區(qū)域季節(jié)氣象模型Multiscan
只是顯飛行航路的雷雨脅與波音的Dark,Quiet
Cockpit概念相符全球氣象模型數(shù)據(jù)庫
(基于氣象領(lǐng)域已建立的成
氣象模型)全球氣象模型數(shù)據(jù)庫的補償Gain
automatically
compensate
for
weather
variations
caused
by
varying
geographic
andclimatic
conditions.(雷雨的含水反射率隨地域及季節(jié)會產(chǎn)生很大的變化,含水反射率不能體現(xiàn)雷雨的
,如對流活動及閃電)The
result
is
the
and
Only
Radar
that
provides
world
wide
hazarddetection.Captain's
Window Officer’s
WindowMultiScanLow
ReflectivityOceanic
WeatherGulf
of
Thailand灣區(qū)域的低反射氣象圖象依此為傳統(tǒng)人工模式,人工最大增益模式及自動模式自動模式在低發(fā)射率的區(qū)域環(huán)境下會自動調(diào)高機器靈敏度,能看到傳統(tǒng) 所無法體現(xiàn)的氣象的整體情況Automatic
Gain
inAutoAUTOCAL
Gain
Gain
alsoadjusted
upon
the
geographical
regionMANUALCAL
GainMANUALMAX
GainOutsideForwardRight自動與人工模式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.地面雜波的顯示是很好的確認(rèn) 工作性能的方法Aviation
Weather航空氣象ReflectivityWet
HailDry
SnowRainDry
Hail提示:AirborneRadar
isDesigned
todetect
rain依靠探測雷雨中含水(降雨)量的多少來工作的,回波與雨量成正比;
無法
探測雪,霧,含水率低的云,干性湍流,閃電,區(qū)分冰雹與降雨的差別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探測局限性系統(tǒng)是機組繞飛雷雨的輔助工具目前工業(yè)界采用的三種顏色級別顯示無法定量的提示無法直接探測閃電的活動人工模式或傳統(tǒng) 為單純的雨量探測自動模式通象模型數(shù)據(jù)庫建立雨量與(對流,閃電)在不同地域及季節(jié)的對應(yīng)關(guān)系,通過顏色的補償會提高對氣象的提示雷雨的濕頂與目視頂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異,會造成傳統(tǒng) 在高空飛行回波弱的感覺,低空回波強的感覺,Multiscan在自動模式下會根據(jù)氣象模型數(shù)據(jù)尤其在雷雨距離飛機較近的情況下(40海里以內(nèi)),波束較細,未能進行較佳的俯仰調(diào)節(jié) 庫判斷雷雨的實際
頂部,體現(xiàn) 氣象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.
成長上升過程20-30米/秒雷雨的不同發(fā)展階段具有不同的 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.雷雨的運動方向受10000英尺中高度風(fēng)的影響雷雨的動態(tài)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統(tǒng)Key
ElementsReceiver/TransmitterAntennaRadomeControl
PanelDisplayPeripheralsIRS/ADC/LRA/Discretes天線俯仰角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
?
increment
or
?
incrementbetween
+/-5
degree
and
?
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.天線穩(wěn)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)增益及校準(zhǔn)增益Calibrated
Gain人工模式CAL=降雨反射率自動模式CAL=降雨反射率+基于溫度的自動補償+全球氣象模型數(shù)據(jù)庫的補償注:人工模式
通過顏色級別來顯示雷雨的強弱,但顏色的等級與閃電的活動和氣流的強烈并無正比關(guān)系,很多情況,綠色(新形成的雷雨)可能會伴隨著頻繁的閃電活動和氣流(顛簸)的運動。CAL增益下雷雨強度與顏色級別的對比關(guān)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亮帶(負增益的使用)Bright
Band(Bright
Band/RedOut)全紅現(xiàn)象全紅產(chǎn)生的兩個原因大面積強降雨包含大尺寸的雨滴大面積層云零溫度線下產(chǎn)生亮帶層次(雪包著水),亮帶以下可能只為輕雨或小雨(飛機下降至亮帶以下, 波束如離開亮帶,全紅的現(xiàn)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距飛機越近,波束越窄,掃到雷雨的切面越薄, 的信息點越多,顯示雷雨的分辨率越好距飛機越遠,波束越寬,更容易掃到雷雨,但雷雨的分辨率差發(fā)出的波束為3.5發(fā)散角的圓錐體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.結(jié)論距離越遠,波束越寬,
分辨雷雨細節(jié)的能力越差建議80nm以內(nèi)對目標(biāo)進行分析80nm以外的顯示主要作為確認(rèn)目標(biāo)的位置與存在及進行飛行計劃Beam
Characteristics
&
Attenuation隨著飛機與雷雨的相對靠近,由于波束變細和波束能量距離傳遞損耗的減少,雷雨的細節(jié)更清楚,尺寸有所增長,綠色增加是正?,F(xiàn)象STC的有限調(diào)節(jié)能力(40海里以內(nèi))TimeReceiver
Sensitivity隨著飛機接近云間通道,波束能量衰減減少,綠色可能逐漸充溢通道(自動模式)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(自動模式失效,可選擇人工模式使用)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: 有嚴(yán)格的 電路,如反射功率等的降低到一定門限,會觸發(fā)WXRFAIL,說明 失效,一般情況下,不要輕易認(rèn)為 回波弱,功率不夠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:(自動模式失效,可選擇人工模式使用)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自動模式失效,可選擇人工模式使用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,當(dāng)選擇自動模式時,
需要進行4個掃描起始過程
2,在正常自動模式的工作狀態(tài)下,如在短時間內(nèi)選擇人工方式(38秒內(nèi)),再轉(zhuǎn)回自動模式,因為
了先前的自動設(shè)置,所以不需再進行起始過程.對安裝雙套
系統(tǒng)的情況,由原正常工作的系統(tǒng)轉(zhuǎn)化至另套系統(tǒng)也需經(jīng)過起始顯
示地面雜波的過程自動模式的自動調(diào)節(jié)補償,抑制地面雜波Auto
Alignment
Process現(xiàn)象:自動模式爬升或巡航階段觀察到地面雜波(一般在80海里左右或以外),原因:在更換
R/T或 驅(qū)動器之后,
需在第一次飛行的巡航高度,自動調(diào)整以補償系統(tǒng)安裝誤差及飛機在空中結(jié)構(gòu)彎曲變化造成對零參考面的影響,以實現(xiàn)高精度的波束俯仰角度,用以計算地面雜波的濾除.調(diào)整過程中雜波的出現(xiàn)并不影響中近程雷雨的探測,同時也可按需使用人工方式調(diào)整過程的實現(xiàn)需要在飛機進入平飛狀態(tài),巡航高度,陸地飛行的情況下進行,一般需要幾分鐘的時間.調(diào)整結(jié)束后地面雜波完全濾除,此種情況下
的工作完全正常.Auto
Mode
Ground
Clutter
Suppression
RequiresPrecise
Knowledge
of
Radar
Antenna
Position雜波抑制需知道天線波束的精確俯仰角度Antenna
Drive,
IRS
Installation
Variations天線驅(qū)動器和慣導(dǎo)系統(tǒng)的安裝差異Aircraft
Flex
in
Flight
(transition
from
groundstatic
calibration)飛機結(jié)構(gòu)在空中的柔性變化對零參考線的影響Auto
Alignment
Process
in
cruise
will
compensatefor
these
variations在巡航平飛開始后會進行自我調(diào)整(幾分鐘),補償上述誤差,雜波的出現(xiàn)并不影響中近程雷雨的探測,同時也可使用人工進行確認(rèn)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飛躍保護在22000ft啟動會
低于飛行高度約6000ft的雷雨(雷雨反射體的頂部與飛機的相對高度),并始終保持在顯示器上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自動模式只顯 脅飛行航路的雷雨,避免不必要的干擾建議由巡航轉(zhuǎn)入下降前從自動轉(zhuǎn)化至人工模式調(diào)低天線角度,觀察低空雷雨的情況隨著飛機的逐步下降,再轉(zhuǎn)回自動模式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)如對自動模式有疑問,人工模式可隨時選擇,人為的控制俯仰,搜索雷雨的反射體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(掃描地波毛邊)(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基于掃描地波毛邊的俯仰設(shè)置理念,大幅調(diào)低天線,再慢慢調(diào)起Tilt
Management(掃描地波毛邊)(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探測的死角(雷雨與飛行高度接近)Tilt
Management(掃描地波毛邊)(Guidelines)不同距離圈設(shè)置的掃毛邊圖示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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