Wind Field Observations with a Monostatic and Bistatic C ... - WakeNet
Wind Field Observations with a Monostatic and Bistatic C ... - WakeNet
Wind Field Observations with a Monostatic and Bistatic C ... - WakeNet
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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