The Wind-Wave Tank of the University of Hamburg

At U Hamburg's wind-wave tank basic research is perfomed on air-sea interactions and their remote sensing. Fluxes of energy, momentum, gas and heat, along with the underlying small-scale processes, can be varied and studied. Frequent experimental campaigns are performed aid in the development of new theories on air-sea interactions and on the radar remote sensing of wind-roughended sea surfaces.

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• U Hamburg's wind-wave tank.
  
  

The wind_wave tank was built in the early 1970s and is located in a hall at the Federal Institute of Waterways Engineering in Hamburg-Rissen. The water-filled part of the large facility is 24 m long and 1 m wide, and the air volume is 1 m high. The tank is filled with fresh water, a radial blower is used to generate wind speeds up to 25 m/s and a wave flap to generate long waves of frequencies between 0.7 Hz and 2.5 Hz.

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• Schematic side view of the wind-wave tank during campaigns with artificial rain; 1: wind tunnel; 2: beach; 3: radar antennas; 4: wave height and slope sensors; 5: laser optics; 6: rain generator; 7: honeycomb; 8: wave flap; 9: radial blower.
  
  

The wind-wave tank is very well suited for experiments under controlled environmental conditions. E.g., in order to simulate biogenic films on the sea surface chemical model substances can be deployed, which form surface films of only one molecule thickness. The impact of those films on the small-scale wave and current field, and on the backscattered radar power, can be studied in great detail. Taking advantage of its flexible usage, the wind-wave tank can be well used to study a wealth of scientific aspects and to help in interpreting remotely sensed data.

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• Photographs showing the damping effect of a surfactant; left: wind-generated waves at 5m/s; right: same wind speed, but upper part covered by a surfactant.
  
  

In the late 1990s, a rain generator was developed and installed to generate heavy rain of up to 300 mm/h on an area of 2.3 m². In the mid 2000s, an air re-circulation was added for comprehensive gas exchange measurements.

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• Photograph showing splash products caused by impinging rain drops.
  
  

Since the mid 1980s, dedicated experiments at U Hamburg's wind-wave tank have been used to generate a better understanding of the radar backscattering from the ocean surface. The radar backscatter depends on the surface roughness, which is a function of wind speed, but which may also be increased by heavy rain, or decreased by marine surface films. Those effects can well be simulated in the wind-wave tank of the University of Hamburg.

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• Synthetic Aperture Radar (SAR) Image of the South China Sea, acquired from the European ERS-1 satellite on 14 May 1998 at 02:52 UTC ((c) ESA). Bright patches in the lower left part were caused by heavy rain, the elongated dark patches in the upper left part by marine surface films. Image size 100 km x 110 km.
  
  

More recently, dedicated experiments on turbulent flows on either sides of the wind-roughened water surface were performed, deploying state-of-the-art laser sensors. Experiments with a Laser Doppler Velocimeter (LDV) allowed measuring time series of two-dimensional currents in the air and upper water layer, just millimeters above and below the water surface, respectively.

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• Photograph taken during measurements with the Laser Doppler Velocimeter.
  
  

The knowledge of small-scale processes at wind-roughened water surfaces is key to our undertanding of exchange processes across the water surface, including the transfer of so-called greenhouse gases. When a fluorescent dye is added to the water in the wind-wave tank, detailed studies of the dynamic water surface can be performed. Laser-Induced Fluorescence (LIF) uses a laser-generated light sheet to visualize the two-dimensional surface of wind-generated waves. Deploying high-speed cameras we monitor the generation of gravity-capillary waves, along with small-scale breaking events that give rise to changes in the wave spectra and in the local air and water flows in the vicinity of the water surface.

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• Laser-Induced Fluorescence (LIF) measurements of a wavy water surface.
  
  

Particle Image Velocimetry (PIV), in combination with LIF, provides high-resolution measurements of velocity fields and underwater turbulent dynamics within the first millimeters above and below the water surface in the presence (and absence) of surfactants. At the wind-wave tank of the University of Hamburg we jointly use PIV and LIF techniques, along with various wave height and slope sensors, to get a full picture of the turbulent dynamics above and below the wavy water surface.

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• Particle Image Velocimetry (PIV) measurements in U Hamburg's wind-wave tank.
  
  

Description

• Description of UHH's wind-wave tank (M. Gade, 2003)

Previous Research

• Sea slicks and their chemical properties

• Gas transfer across the water-air interface

• Monomolecular surface films: wave damping and radar backscattering

• Bound and free gravity-capillary waves

• Experiments with heavy rain

• Rain-induced sub-surface turbulence

Ongoing Research

• Momentum and energy fluxes

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