Showing posts with label Petermann Glacier. Show all posts
Showing posts with label Petermann Glacier. Show all posts

Wednesday, March 19, 2014

ESA Sentinel-1A: Preparation for radar vision

This ‘interferogram’ shows Petermann Glacier grinding towards the sea along the northwestern coast of Greenland. 

Two Radarsat-2 TOPS images acquired 24 days apart were used to generate it. 

Radarsat-2 was programmed specially by MDA to work in an experimental imaging mode called Terrain Observation by Progressive Scans (TOPS) in azimuth to match the way ESA’s Sentinel-1 will image Earth. 

Credit: ESA/MDA

Sentinel-1A, Europe's first satellite for Copernicus, is almost ready for launch on 3 April. Meanwhile, ESA is showing how its advanced radar will map ice, monitor subsidence and much more.

Marking a new era in Earth observation focusing on operational applications, Sentinel-1A is set to deliver timely imagery for numerous Copernicus services.

Carrying an advanced radar, it will scan Earth's surface no matter what the weather and regardless of whether it is day or night.

In crisis situations, it will be used for rapid response to disasters such as floods and earthquakes. Its radar will routinely monitor shipping zones, map sea ice and provide information on winds and waves for marine traffic, track changes in the way land is being used, and monitor subsidence.

It will also track how glaciers move, as shown in the image above of Petermann Glacier in northwest Greenland.

So that users are fully prepared for the images Sentinel-1A delivers, Canada's Radarsat-2 was recently programmed by MacDonald, Dettweiler & Associates to scan Earth's surface using the same novel 'interferometric' wide-swath mode technique as Sentinel-1.

Consequently, a suite of images was acquired over various sites.



Carrying an advanced radar, Sentinel-1A can image Earth’s surface no matter what the weather and regardless of whether it is day or night. 

This makes it an ideal mission for monitoring the polar regions, which are shrouded in darkness for months at a time. 

As well as providing information on changing ice cover and glacial flows, Sentinel-1 will provide imagery of sea-ice for maritime navigation in polar waters. 

Sentinel-1A will also be used to track changes in the way land is used and to monitor ground movement. 

Moreover, this new mission is designed specifically for fast response to aid emergencies and disasters such as flooding and earthquakes. 

Sentinel-1A, the first in the family of satellites for Europe’s environmental monitoring Copernicus programme, marks a new era in Earth observation, focusing on operational missions to support users for decades to come. 

Credit: ESA/ATG medialab

As the most realistic Sentinel-1A-like images to date, they show the performance and suitability of the new mission for classifying different types of sea ice, detecting ships and monitoring oil platforms.

They also included image pairs to show changes in glaciers such as Petermann, and a 'stack' of 11 images to map surface subsidence in Mexico City.

The image of Petermann Glacier was derived from two images taken 24 days apart. It shows some stationary and slowly moving features, as well as some large areas of much faster-moving ice.

The pattern's fringes are widely spaced in the stationary areas and closer together in the centre of the glacier where the ice is moving much faster.

The wealth of data available through ESA's Earth observation campaign data website is helping to pave the way for users to get the maximum out of the upcoming mission.

The Sentinel-1mission comprises two identical satellites for optimal global coverage and data delivery.

Sentinel-1B will join Sentinel-1A in orbit next year.

Thursday, July 19, 2012

NASA - Petermann Glacier, Greenland

The Petermann Glacier grinds and slides toward the sea along the northwestern coast of Greenland, terminating in a giant floating ice tongue.

Like other glaciers that end in the ocean, Petermann periodically calves icebergs.

A massive iceberg, or ice island, broke off of the Petermann Glacier in 2010. Now, nearly two years later, another chunk of ice has broken free.

The Moderate Resolution Imaging Spectroradiometer, or MODIS, on NASA’s Aqua satellite observed the new iceberg calving and drifting downstream on July 16–17, 2012. Because Aqua is a polar-orbiting satellite, it makes multiple passes over the polar regions each day.

Image Credit: NASA

Wednesday, August 11, 2010

ESA ENVISAT ASAR: Greenland glacier gives birth to giant iceberg


Time-series animation based on Envisat Advanced Synthetic Aperture Radar (ASAR) data from 31 July, 4 August, and 7 August 2010 showing the breaking of the Petermann glacier and the movement of the new iceberg towards Nares Strait.

Credits: ESA



True-colour Envisat MERIS image of Petermann glacier on 5 August 2010 showing the iceberg already separated from the main glacier tongue. Cloud coverage prevents obtaining additional MERIS images spanning the actual calving event.

Credits: ESA

To read the full article Click here

Monday, August 9, 2010

NASA MODIS: Ice Island of Petermann Glacier

On August 5, 2010, an enormous chunk of ice, roughly 97 square miles (251 square kilometers) in size, broke off the Petermann Glacier, along the northwestern coast of Greenland.

The Canadian Ice Service detected the remote event within hours in near real-time data from the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite.

The Peterman Glacier lost about one-quarter of its 70-kilometer (40-mile) long floating ice shelf, said researchers who analysed the satellite data at the University of Delaware.

The Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite captured these natural-color images of Petermann Glacier 18:05 UTC on August 5, 2010 (top), and 17:15 UTC on July 28, 2010 (bottom).

The Terra image of the Petermann Glacier on August 5 was acquired almost 10 hours after the Aqua observation that first recorded the event. By the time Terra took this image, skies were less cloudy than they had been earlier in the day, and the oblong iceberg had broken free of the glacier and moved a short distance down the fjord.

Icebergs calving off the Petermann Glacier are not unusual. Petermann Glacier’s floating ice tongue is the Northern Hemisphere’s largest, and it has occasionally calved large icebergs. The recently calved iceberg is the largest to form in the Arctic since 1962, said the University of Delaware.

Friday, March 26, 2010

NASA Goddard Blog: Operation Ice Bridge

Operation IceBridge Off to a Successful Start in Greenland

Credit: Michael Studinger
The IceBridge crew fly down Petermann Glacier in northern Greenland with NASA's DC-8 aircraft.