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 |