Instrumentation Table |
|||||
VARIABLE |
INSTRUMENT |
RANGE |
ACCURACY |
RESOLUTION |
NOTES |
Static
Pressure |
Rosemount
1301-A-4B |
0-15 psi
(0-103 kPa) |
±0.015 psi |
0.0002
psi |
|
|
Rosemount
1301-A-4B |
5-15
psi (35-103 kPa) |
±0.015 psi |
0.0002
psi |
|
Total
Temperature |
Rosemount
102AU2AP |
-30
to +30°C |
±0.5°C |
0.001°C |
·Platinum wire ·2 s time constant |
|
NCAR
Reverse Flow |
-30
to +30°C |
±0.5°C |
0.001°C |
·Platinum RTD element ·Several seconds time
constant |
Cloud
Water and |
DMT
Liquid Water |
0
- 4 g/m3 |
±20% |
0.0001
g/m3 |
·Sampling rate 4 l/km |
|
Particle
Measuring Systems, Inc. Forward Scattering Spectrometer Probe |
Size
1 < 67 mm 0
- 2000 droplets/cm3 |
±1 size channel in size and ±1% in concentration at ~50/cm3 |
1
size channel |
·15 discrete size channels
spread over an adjustable range ·Sampling rate 300 cm3/km
·Accuracy of computed liquid
water concentration ~±50%. Depends on processing. |
Precipitation
Particle Sizes And Concentrations |
Particle
Measuring |
Size
25 - 800 mm |
±25 mm |
25
mm |
·Computed ice and water mass
concentration can vary ±50% with processing
technique ·Sampling rate: 0.05 m3/km;
DAS can accept ~250 particles/s (2500/km) |
High-Volume
Particle Sampler |
SPEC HVPS |
Size
0.2 – 50 mm |
±0.2 mm |
0.2
mm |
·Sampling rate: 10 m3/km ·Also senses particle
electric charge |
|
Hail
Spectrometer |
Size
4.5 mm - 4.5 cm Concentration 0 - 100/m3 |
±1 size class |
1
size class |
·14 size classes, and images
·Sampling rate 100 m3/km |
Aircraft
Motion |
Humphrey
|
±2 g's |
0.004
g's |
0.00006
g |
|
|
Rosemount
1301-D-1b |
|
±0.1% |
0.0001
psi |
|
|
Rosemount
1221-F-2A |
–2.5
to +2.5 psi |
±0.1% |
0.0001
psi |
|
|
Giannini
45218YE |
0
to 50 in Hg |
±2% |
0.008
Hg |
·Used in backup vertical
velocity calculation |
|
Crossbow
Non-Stabilized 3-Axis Accelerometer |
±4 g in all 3 directions |
±0.2% |
3.05
x 10-4 g's |
|
Aircraft
Location |
Trimble
TNL2000 GPS |
(global) |
30
m |
18
m |
|
Electric
Field |
NMIMT
Model E-100 |
top/bot
± 650 |
|
(coarse
resolution) |
|
NOTE: Many of these instruments do not behave as
ideal instruments. The use of one measure of accuracy over the entire range
of measurement is, in many cases, questionable. An accuracy representative of
the most useful part of the range is given here.
Revised
01/2001 |