Aerial observations

 

A crucial element of SHEBA is to extend process-oriented observations and models to larger-scales. Local measurements provide data on mass changes, optical properties, and structural properties of individual ice categories, and ground surveys allowed us to define spatial variability within each category. We then use larger scale aerial surveys to generate regional estimates of the fractional area covered by these categories. Combining these observations with process-oriented modeling results makes it possible to generate areally averaged estimates of such quantities as albedo, solar heat input to the ice and ocean, ice concentration, pond fraction, and lateral melt rates.

Between May and October 1998 more than a dozen helicopter survey flights were made. An instrument package consisting of a Nikon 35-mm camera, a videocamera, and a KT-19 thermal radiometer was mounted, in a downward-looking orientation, on the back of the helicopter's storage compartment. Whenever possible surveys were flown at an altitude of 6000 ft under either clear skies or high clouds. The flight pattern was a box centered on the Des Groseilliers. The first leg was 25 km east followed by 25 km due north, 50 km due west, 50 km south, then 25 km east, and finally 25 km north back to the ship.

Photographs

Surface temperature

Helo albedos

Helo areas

Helo logs

 

 

From left to right the instruments are Nikon 35-mm camera with film pack and motor drive, KT-19 thermal radiometer, Hi-8 video camera, and downwarding-looking spectroradiometer.

Helicopter doing airborne oceanography.

 

Instrument package mounted on edge of helo storage compartment.

 

 

 
                                          

Home

Optics

Mass

Snow

Aerial

Logs