sbi-2005 1/13 vagarities of velocity variations andreas muenchow graduate college of marine studies...
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SBI-2005
1/13
Vagarities of Velocity Variations
Andreas Muenchow
Graduate College of Marine Studies
University of Delaware
http://newark.cms.udel.edu/~sbi
Chr
is L
inde
r, W
HO
I
SBI-2005
2/13
• transmits sound then listens for echoes
• sound interacts with ~ 2-cm particles (zooplankton)
• backscattered sound received by transducers
Velocity:Radar + Sonar
Radar send and receiveelectromagnetic waves (radio, police)
Sonar send and receives acoustic waves (sound, whales)
Same physics.
75-kHz transducers:
SBI-2005
3/13
Zooplankton diel vertical migrations?
ADCP backscatter Beaufort slopeOct.-2004
~10 m/hr~0.28 cm/s
SBI-2005
4/13
Aagaard (1984)
SBI-2005
5/13
cm/s
Beaufort Slope Currents 2003
SBI-2005
6/13
Beaufort Slope Currents 2004
SBI-2005
7/13
•
•
t0
t0+16 hrs
east west
L
Barrow Canyon, Sept. 1993
Synoptic velocity observation in Barrow Canyon, Alaska(view is to the south):
The flow scales with the internal deformation radius, L~5-km.
Münchow and Carmack (1996)
SBI-2005
8/13
Barrow Canyon 2004
Barrow Chukchi
SBI-2005
9/13
Coastal Circulation off Wainwright,Sept.-12, 2004
as measured by75-kHz acoustic Doppler current profiler
Flow is in the opposite direction from what is the canonical view of fresh Bering Sea water entering the Arctic via Barrow Canyon
SBI-2005
10/13
I
II
III
Eddies in the ArcticSept.-22, 2004
I II III
USCGC Healy 75-kHz ADCP
L
D
SBI-2005
11/13
The only real SBI-ADCP Survey, Sept.-22/24, 2004
55-m 100-m
red dots are XBT drops (Pickart and Kosro)
Chukchishelf
Chukchishelf
SBI-2005
12/13
Warm, fresh water flows northward against gale force winds in channel while
cooler and saltier waters flow southward with the winds.
Central Channel Chukchi Shelf8-m temperature
8-m salinity
SBI-2005
13/13
How to best distribute ADCP data?How to best “explore” ADCP data?
file:///Users/a2/0309_pro/os75/www0309/index.html
Conclusions:•ADCP velocity data challenges conventional perceptions of Arctic shelf and slope circulations (strong vs. weak local forcing);
•SBI did not resolve velocity and physical property fields properly in time-space domain (with the exception of WHOI moored array)
Questions:
SBI-2005
14/13
ADCP Processing: Sorting and Screening Single Ping Data
water trackrelative to ship(true East, unsorted)
water trackrelative to ship(true North, unsorted)
water trackrelative to bottom(true North, sorted)
water trackrelative to bottom(true East, sorted)
Ensemble average
Ensemble
SBI-2005
15/13
ADCP Calibration-1:Comparing Velocity Components
… looks good,but can’t tellhow good …
Transducer misalignment in
x-y plane: 44.1 deg.
x-z plane: 1.17 deg.
y-z plane: -1.10 deg.
Scaling by 1.021158
SBI-2005
16/13
ADCP Calibrations-2:Difference of ADCP-GPS Velocity Components
North
East
Histogram Integrated Histogram
SBI-2005
17/13
Barotropic Tidal Currents5-km data assimilation8 constituents, 2-week rms
from Erofeeva et al. (2004)