The biggest dust storm ever seen over Greenland has been revealed in a series of stunning satellite images. The unusual event is caused by 'glacial flour', a fine-grained silt formed by glaciers grinding and pulverizing rock. Scientists have never been able to study the phenomenon in large storms until last month, when satellite images captured a storm.
'This is by far the biggest event detected and reported by satellites that I know about,' said Santiago Gassó, an atmospheric scientist at NASA's Goddard Space Flight Center. He first noticed the storm on October 3.
Joanna Bullard of Loughborough University said: 'We have seen a few examples of small dust events before this one, but they are quite difficult to spot with satellites because of cloud cover. When dust events do happen, field data from Iceland and West Greenland indicate that they rarely last longer than two days.'
The Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA's Terra satellite and a sensor on the European Space Agency's Sentinel-2 collected the first imagery of the storm on September 29, 2018, showing a sizable silt plume streaming from Greenland's east coast. The source was a braided stream valley about 130 kilometers northwest of Ittoqqortoomiit, a village at a latitude of 73 degrees North. That puts the village north of the northern coast of Alaska.
The series of Landsat and Sentinel 2 images show the floodplain where the stream flows into Scoresby Sound. As the soil on the floodplain dried out, the floodplain became increasingly gray. Northwesterly winds on September 29 were strong enough to lift glacial flour into the air. The glacial flour was likely made by several glaciers farther up the valley, then carried south by meltwater streams and deposited in the floodplain. As stream water levels dropped in autumn, the floodplain dried out and became susceptible to scouring by the wind.
In this case, Bullard noted, the winds were triggered by the combination of a low-pressure system crossing the Greenland ice sheet followed closely by a ridge of high pressure. Since high-latitude dust events are poorly understood, they are typically not included in atmospheric and climate models. Gasso hopes that eventually they will be included because they could have effects on air quality, the reflectivity of snow, and even marine biology.
Extracted from: www.dailymail.co.uk