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Remote Sensing Global Surface Air Pressure using Differential Absorption BArometric Radar (DiBAR) Bing Lin 1 , Steven Harrah 1 , Wes Lawrence 2 , Yongxiang Hu 1 , and Qilong Min 3 1 NASA Langley Research Center, Hampton, VA 2 Old Dominion University, Norfolk, VA 3 State University of New York, Albany, NY International Radiation Symposium 2016 16-22 April 2016, Auckland, New Zealand https://ntrs.nasa.gov/search.jsp?R=20160009261 2018-06-01T06:35:45+00:00Z

Remote Sensing Global Surface Air Pressure using ... · Air Pressure using Differential Absorption BArometric Radar (DiBAR) Bing Lin1, ... Aircraft/Spacecraft-Based Q-Band ... Day

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Remote Sensing Global Surface Air Pressure using Differential

Absorption BArometric Radar (DiBAR)

Bing Lin1, Steven Harrah1, Wes Lawrence2, Yongxiang Hu1, and Qilong Min3

1NASA Langley Research Center, Hampton, VA2Old Dominion University, Norfolk, VA

3State University of New York, Albany, NY

International Radiation Symposium 2016

16-22 April 2016, Auckland, New Zealand

https://ntrs.nasa.gov/search.jsp?R=20160009261 2018-06-01T06:35:45+00:00Z

• Develop satellite capability of

Surface Level Pressure (SLP)

observations, especially over oceans

• Global SLP measurements will:

- greatly improve hurricane forecasts

(intensification & track predictions)

- advance severe weather forecasts

- directly measure the fundamental

variable of meteorological dynamics

• Current: develop Proof-of-Concept

(PoC) system, demonstrate the

Differential absorption BArometric

Radar (DiBAR) technology using

PoC system for SLP measurements

Objectives(Dynamic fields, hurricanes)

Benefits of sea surface barometry

actual

track

with P

data

Control

Fran’97Hurricane Katrina

Aug 26, 2005

Aug 29, 2005

Min et al., 2014

350 km landfall error

reduced to < 100 km

Spatial coverage: very limitedCosts: highBuoy: uncertain in hurricanesUncertainty: ~1 mb

Existing techniques: in-situ

drift buoy

moored buoy

dropsonde

No remote sensing technique is available.

Current Capability

In-Situ Sea Surface Air Pressure Measurements for Weather Forecasts and Atmospheric Dynamics

Atmospheric attenuation

Frequency (GHz)70

0.1

300

Att

enuat

ion (

dB

)

1

10

100

50 54 58 62 66

Oxygen in the atmosphere

attenuates the transmitted signal

– less at lower freq. and

more at higher freq.

The amount of attenuation

is directly related to

barometric pressure and altitude.

f or 1/l (50~55GHz)

PRec

Atte

nuatio

n

Calibrated PRec

w/o Attenuation

Aircraft/Spacecraft-Based

Q-Band (50-55GHz) Radar

Measurement Concept

Simulated barometry results

Lin and Hu, 2005 Global weather conditions

PoC Instrument developed

Agilent

8362B

PNA

50-56 GHz Transceiver

15 GHx PLO

X 5 = 45GHz

Port 1

Port 2

10 MHz Ref

5-11 GHz IF

5-11 GHz IF 50-56 GHz

Transmit

Antenna

Receive

Antenna

5-11 GHz IF

5-11 GHz IF

15 GHz PLO

50-56 GHz

Agilent

8362B

PNA

50-56 GHz Transceiver

15 GHx PLO

X 5 = 45GHz

Port 1

Port 2

10 MHz Ref

5-11 GHz IF

5-11 GHz IF 50-56 GHz

Transmit

Antenna

Receive

Antenna

5-11 GHz IF

5-11 GHz IF

15 GHz PLO

50-56 GHz

Agilent 8362B

Network Analyzer

SpaceK Labs

45GHz Up/Down

Converter

Quinstar 24"

Cassegrain Antennas

Simplified PoC Instrument

Thursday, November 13, 2008 10:30 am EST

DiBAR flight results

50 51 52 53 54 55 56 57 58 59 60-80

-75

-70

-65

-60

-55

-50

Frequency (GHz)

Radar

Retu

rn (

dB

)

Day 1, Day 2, & Day4

1007 mb

1018 mb

1028 mb

3000 ft

Increased O2 absorption

loss vs. frequency

evident for all flight

measurements.

Differential absorption,

or Ri, shows correlated

with increasing SLP for

the flight campaign data.

The measured differential loss validated the predicted frequency

dependence and was clearly correlated with surface level pressure.

50 52 54 56 58 60-25

-20

-15

-10

-5

0

Frequency (GHz)

Ri(

alt

)/R

i(5

00

ft)

DiBAR Flight Test LANGLEY

RESEARCH

CENTER

Differential absorption

was measured for 0 – 2

km altitudes.

Results are consistent

with O2 absorption model.

Sensitivity to surface

barometric pressure

demonstrated.

+ Ri(2000)/Ri(500)

Ri(3000)/ Ri(500)

+ Ri(2000)/Ri(500)

Ri(3000)/ Ri(500)

Ps=1018 mb

Ps=1028 mb

+ 2000 ft

3000 ft

SLP=1018 mb

SLP=1028 mb

Psurface = 10 mb

Radar Sea Level Pressure Remote Sensing for

Improvements in Hurricane Predictions

±10o

LEO (705 km)

DiBAR

Satellite Concept

Torbit ~98 min

250 km

~ 1/6 o

2 km

Design Est.:

Mass: 250kg

Power: 250W

& DL Comm.

FY -- TBD

Summary

The differential O2 absorption approach will provide the first remote sensing barometric data over the globe!

The accuracy of instantaneous sea surface air pressure measurements from O2-band sensors could be as high as ~4 mb.

DiBAR technology will lead significant improvements in predictions of hurricane intensities and tracks and provide great benefits for the public.

Operational capability of DiBAR approach potentially enables the monitoring of changes in the extreme storm and precipitation events such as tropical storms, and has both weather and climate applications.

The SLP measurement approach will dramatically extend the current, limited-point barometric measurements to global observations for tropical storm forecasts when spaceborne instruments are available.