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<strong>Wind</strong> <strong>Field</strong> <strong>Observations</strong> <strong>with</strong><br />

a <strong>Monostatic</strong> <strong>and</strong> <strong>Bistatic</strong><br />

C-b<strong>and</strong> Doppler Radar Network<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen<br />

Institut für Physik der Atmosphäre, DLR Oberpfaffenhofen


<strong>Wind</strong> field <strong>and</strong> Doppler radar<br />

Doppler radar (<strong>and</strong> lidar) can only measure one component<br />

(the radial one) of the 3-dimensional wind vector<br />

v r<br />

w<br />

v<br />

u<br />

-16 0 m/s 16<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

2


<strong>Wind</strong> field <strong>and</strong> Doppler radar<br />

Estimation of the 3-dimensional<br />

single Doppler wind field techniques (VAD, VVP, UWT, ...)<br />

make assumptions about the<br />

wind field (linear, homogeneous,<br />

constant) <strong>with</strong>in a region<br />

(dimension of several kilometres)<br />

requires more than one radar<br />

(or lidar)<br />

vertical air motion can not be<br />

retrieved, it will be estimated by<br />

vertical integration of convergences<br />

of the horizontal wind field (3d-var, 4d-var techniques)<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

3


<strong>Monostatic</strong> <strong>and</strong> <strong>Bistatic</strong> Doppler Radar Network<br />

<strong>Monostatic</strong> radar network:<br />

same antenna for<br />

transmit <strong>and</strong> receive<br />

<strong>Bistatic</strong> radar network:<br />

different antennas for<br />

transmit <strong>and</strong> receive<br />

<strong>Bistatic</strong><br />

Receiver<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

4


<strong>Monostatic</strong> Doppler Radar Network<br />

<strong>Monostatic</strong> radar network:<br />

same antenna for<br />

transmit <strong>and</strong> receive<br />

minimum 2, better more radars (or lidars) are required<br />

synchronized scanning<br />

short distance (20 – 40 km) between radars to<br />

cover low-level wind field features close to the<br />

airport (operational networks: distance 100 - 200 km)<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

5


<strong>Monostatic</strong> Doppler radar network<br />

Estimation of horizontal wind vector<br />

<strong>with</strong> measurements from two<br />

Doppler radars<br />

Highest accuracy if intersection<br />

angle γ = 90°<br />

Sufficient accuracy for 30° < γ < 150°<br />

St. dev. hor. wind (m/s)<br />

10<br />

8<br />

6<br />

4<br />

2<br />

0<br />

0 30 60 90 120 150 180<br />

Intersection angle (°)<br />

assumed st. dev. of Doppler velocity 1 m/s<br />

Radar 2<br />

90°<br />

Basislinie<br />

120°<br />

Radar 1<br />

60°<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

6


<strong>Monostatic</strong> <strong>and</strong> <strong>Bistatic</strong> Doppler Radar Network<br />

<strong>Bistatic</strong> radar network:<br />

different antennas for<br />

transmit <strong>and</strong> receive<br />

<strong>Bistatic</strong><br />

Receiver<br />

<strong>Bistatic</strong> radar network uses one active (transmit <strong>and</strong> receive) radar<br />

<strong>and</strong> several passive receivers<br />

measurements are synchronized in time <strong>and</strong> space<br />

bistatic receivers are cheap (0.1 vs. 1.5 M€)<br />

distance between receivers – radar: 20 – 40 km<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

7


<strong>Bistatic</strong> Doppler radar network<br />

Horizontal wind composed from<br />

radial Doppler velocity measured by radar (v r ),<br />

(elliptical) Doppler velocity measured by bistatic receiver (v e ).<br />

accuracy is reduced since<br />

intersection angle between<br />

v e <strong>and</strong> v r = ½ scattering angle γ<br />

St. dev. hor. wind (m/s)<br />

10<br />

8<br />

6<br />

4<br />

2<br />

0<br />

bistatic<br />

monostatic<br />

assumed st. dev. of Doppler velocity 1 m/s<br />

0 30 60 90 120 150 180<br />

scattering angle (°)<br />

r t<br />

v e<br />

v r<br />

scattering<br />

angle γ<br />

Transmitter<br />

+ Receiver<br />

r b<br />

Receiver<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

8


<strong>Monostatic</strong> versus bistatic Doppler radar network<br />

Reduced accuracy <strong>and</strong> areal coverage can easily be compensated<br />

by a larger number of receivers<br />

monostatic 2 radars bistatic 1 radar 1 receiver bistatic 1 radar 3 receivers<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

9


<strong>Bistatic</strong> Doppler radar network<br />

first trials 1993: NCAR / Univ. of Oklahoma<br />

challenge: synchronization of oscillator at radar <strong>and</strong> remote site<br />

for accurate phase estimation<br />

available systems for research:<br />

McGill University Montreal (1996 – 2002 ?)<br />

first permanent installation, klystron transmitter<br />

NCAR S-Pol radar field campaigns<br />

e.g. IMPROVE I at Pacific coast (2001)<br />

NICT Japan, Okinawa (2003 ?)<br />

C-b<strong>and</strong>, klystron transmitter, GPM ground validation site<br />

DLR Oberpfaffenhofen (1998 – 2005; 2010 - )<br />

first C-b<strong>and</strong> system <strong>with</strong> magnetron transmitter<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

10


Overview of DLR<br />

bistatic radar net<br />

Radar POLDIRAD<br />

<strong>Bistatic</strong> receiver<br />

at radar<br />

Remote bistatic<br />

receiver<br />

Hub:<br />

central processor<br />

<strong>and</strong><br />

communication<br />

POLDIRAD<br />

System<br />

antenna<br />

angles,<br />

trigger<br />

GPS<br />

antenna<br />

Phasedetection<br />

synchronized<br />

<strong>with</strong> GPS signal<br />

local display<br />

phase<br />

of tx<br />

pulse<br />

Radar<br />

data<br />

unit<br />

Radarcontrol<br />

Magnetron<br />

Dopplervelocity<br />

<strong>and</strong><br />

Reflectivity<br />

Receiver at the radar<br />

Doppler<br />

R<br />

velocities<br />

<strong>and</strong><br />

B1 reflectivities<br />

from both<br />

receivers<br />

Realtime<br />

wind<br />

vectors<br />

Central bistatic vector processor<br />

Institut für Physik der Atmosphäre<br />

I, Q<br />

Veloc. Refl.<br />

Radar<br />

antenna<br />

TCP/IP<br />

network<br />

<strong>with</strong> ISDN<br />

routers<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

<strong>Bistatic</strong><br />

antenna<br />

Azim., Elev.,<br />

time, phase<br />

Dopplervelocity<br />

<strong>and</strong><br />

Veloc. Refl. Reflectivity<br />

Phasemeasurement<br />

synchronized<br />

<strong>with</strong> GPS signal<br />

local display<br />

Remote receiver<br />

GPS<br />

antenna<br />

11


<strong>Bistatic</strong> Doppler radar network at DLR Oberpfaffenhofen<br />

Lagerlechfeld<br />

Ri ed<br />

MÜNCHEN<br />

Dual-Doppler<br />

Triple-Doppler<br />

4-Doppler<br />

Oberpfaffenhofen<br />

10 km<br />

20 km<br />

11,7 km<br />

Licht enau<br />

30 km<br />

40 km<br />

50 km<br />

Antenna aperture Horizontal Vertical<br />

Lichtenau 60° 8°, 22°<br />

Lagerlechfeld 60° 8°, 22°<br />

Ried 60° 8°<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

12


<strong>Bistatic</strong> Doppler radar network at DLR Oberpfaffenhofen<br />

Lagerlechfeld Lechfeld<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

13


DLR bistatic Doppler radar network wind synthesis<br />

Doppler velocity radar receiver Lechfeld receiver Ried<br />

receiver Lichtenau<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

14


Observation of thunderstorm outflow<br />

9 July 2002<br />

1557 UTC<br />

Elevation 5.4°<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

15


<strong>Observations</strong> in clear-air echoes<br />

Clear-air echoes give<br />

good radar coverage<br />

at short distances<br />

(~50 km) during<br />

summer (insects)<br />

Minimum detectable<br />

signal of bistatic<br />

receivers is less than<br />

for monostatic radars<br />

due to reduced<br />

antenna gain<br />

~10 vs. 45 dB<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

16


Evaluation of bistatic Doppler wind field<br />

Independent Doppler measurements at Hohenpeißenberg<br />

Vh<br />

BINET<br />

Vr<br />

HP from BINET<br />

Difference<br />

Vr<br />

HP meas.<br />

Friedrich & Hagen, 2004<br />

JTECH, 21, 1840-1854<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

17


Conclusion <strong>Bistatic</strong> Doppler radar network<br />

Advantages:<br />

Low costs for a multiple Doppler radar system<br />

high resolution (pulse volume) wind field estimates<br />

temporal synchronized measurements<br />

Disadvantages:<br />

reduced sensitivity (clear-air observations unlikely)<br />

contamination by<br />

side-lobes of radar<br />

Production <strong>and</strong> support<br />

of systems stopped<br />

Friedrich, 2002, PhD thesis<br />

Institut für Physik der Atmosphäre<br />

Martin Hagen, Wakenet-3 <strong>Wind</strong> Workshop, Palaiseau, 29 - 30 March 2010<br />

18

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