Morning Glory cloud
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The Morning Glory cloud is a rare meteorological phenomenon occasionally observed in different locations around the world. The southern part of the Gulf of Carpentaria in Northern Australia is the only known location where it can be predicted and observed on a more or less regular basis due to the configuration of land and sea in the area. The settlement of Burketown attracts glider pilots intent on riding this phenomenon.
Morning Glory clouds can be observed from Burketown from late September to early November. There are generally only a handful of well formed spectacular clouds during this period at Burketown. During the 2012 season there were only four to be seen from there, but quite a few ragged unspectacular cloud lines were seen. Often they start to break up before arriving at Burketown or pass to the north and only stay well formed over water. In an aircraft there is a significantly better chance of sighting the cloud.
A Morning Glory cloud is a roll cloud, or Arcus cloud, that can be up to 1,000 kilometres (620 mi) long,1 to 2 kilometres (0.62 to 1.24 mi) high, often only 100 to 200 metres (330 to 660 ft) above the ground and can move at speeds up to 60 kilometres (37 mi) per hour. Sometimes there is only one cloud, sometimes there are up to eight consecutive roll clouds.
The Morning Glory is often accompanied by sudden wind squalls, intense low-level wind shear, a rapid increase in the vertical displacement of air parcels, and a sharp pressure jump at the surface. In the front of the cloud, there is strong vertical motion that transports air up through the cloud and creates the rolling appearance, while the air in the middle and rear of the cloud becomes turbulent and sinks.
History of exploration
Unusual cloud formations have been noticed here since ancient times. The local Garrawa Aboriginal people called it kangólgi. Royal Australian Air Force pilots first reported this phenomenon in 1942.
The Morning Glory cloud of the Gulf of Carpentaria has been studied by multiple teams of scientists since the early 1970s. The first studies were published by Reg H.Clarke (University of Melbourne). Multiple studies have followed since then, proposing diverse mathematical models explaining the complex movements of air masses in the region.
The Morning Glory cloud is not clearly understood because their rarity means they have little significance in terms of rainfall or climate.
Regardless of the complexity behind the nature of this atmospheric phenomenon, some conclusions have been made about its causes. Through research, one of the main causes of most Morning Glory occurrences is the mesoscale circulations associated with sea breezes that develop over the peninsula and the gulf. On the large scale, Morning Glories are usually associated with frontal systems crossing central Australia and high pressure in northern Australia. Locals have noted that the Morning Glory is likely to occur when the humidity in the area is high, which provides moisture for the cloud to form, and when strong sea breezes have blown the preceding day.
Scenario for formation
The following is a summary of the conditions that cause the Morning Glory cloud to form in the Gulf of Carpentaria (after hypothesis of R.H.Clarke, as described in 1981). First, Cape York which is the peninsula that lies to the east of the gulf, is large enough that sea breezes develop on both sides. During the day, the breeze from the Coral Sea coast blows in from the east and the breeze from the gulf blows in from the west. The two breezes meet in the middle of the peninsula, forcing the air to rise there and form a line of clouds over the spine of the peninsula. When night comes, the air cools and descends and at the same time a surface inversion forms over the gulf (where air temperature increases with height). The densities in this stable layer are different above and below the inversion. The air descending from the peninsula to the east goes underneath the inversion layer and this generates a series of waves or rolling cylinders which travel across the gulf. These cylinders of air roll along the underside of the inversion layer, so that the air rises at the front of the wave and sinks at the rear. In the early morning, the air is saturated enough so that the rising air in the front produces a cloud, which forms the leading edge of the cylinder, and evaporates in the back, hence forming the Morning Glory cloud. The cloud lasts until the surface inversion disappears with the heating of the day.
This is one scenario that explains the formation of the Morning Glory cloud over the Gulf of Carpentaria, but other explanations have also been proposed.
There are other ways in which Morning Glory clouds form, especially in rarer cases in other parts of the world, but these are far less understood.
Local weather lore in the area suggests that when the fridges frost over and the café tables' corners curl upwards at the Burketown Pub, there is enough moisture in the air for the clouds to form. Reportedly, all winds cease at ground level as the cloud passes over.
One vantage point to see Australia's Morning Glory is from Burketown in the remote Far North Queensland around September and October. Towns in this part of the world are small and far apart, and Burketown has an influx of glider and hang-glider pilots at this time of year.
Other reported occurrences
Although the Morning Glory clouds over the southern part of Carpentaria Gulf are the most frequent and predictable, similar phenomena have occasionally been observed elsewhere, e.g., over central United States, the English Channel, Berlin, Germany, Eastern Russia, and other maritime regions of Australia.
Morning Glory clouds have occasionally been reported in the Sea of Cortez off the Mexican coast. The phenomenon has also been observed from Sable Island, 180 km southeast of Nova Scotia. A Morning Glory also passed through Yarmouth, Nova Scotia in April 2009. In contrast to the Gulf of Carpentaria where the Morning Glory is visible in the morning, those in Nova Scotia have all occurred during the evening. Rare examples have been observed via satellite observation over the Joseph Bonaparte Gulf in the Eastern Kimberley region of Australia as well as over the Arabian Sea. A Morning Glory cloud was observed in 2007 over the Campos dos Goytacazes bay in the state of Rio de Janeiro, Brazil. In August 2011, it happened again over Peregrino Field in South Campos Basin in Brazil. The phenomenon was also recorded on Batroun's shore (Lebanon – Middle East) in September 2004. On 20th November, 2013, a Morning Glory formation formed over the greater Durban area.
- Morning Glory Clouds of the Gulf of Carpentaria. Dropbears.com. Retrieved on 28 December 2012.
- "Morning Glory of Carpentaria Gulf". Wondermondo.
- Betty Mason (29 September 2009). "Weird, Rare Clouds and the Physics Behind Them". Wired. Condé Nast. Retrieved 28 December 2012.
- Gavin Pretor-Pinney (2006). The Cloudspotter's Guide. Hodder & Stoughton. ISBN 0-340-89589-6. Chapter 13, The Morning Glory the cloud that glider pilots surf, pp 283–305
- Menhofer A, Smith RK, Reeder MJ, Christie DR (1997) “Morning-Glory” Disturbances and the Environment in which They Propagate. Journal of the Atmospheric Sciences: Vol. 54, No. 13 pp. 1712–1725
- Smith, Deborah. (2002) Morning Glory lures scientists to ride cloud nine The Sydney Morning Herald. September 16, 2002
- regarding Tropical cloud lines
- morninggloryaustralia.com Meteorological information, photos and video of the Morning Glory cloud.
- hang glider soaring hang gliding on the Morning Glory phenomenon, with aerial photos and videos of the cloud.
- ABC Australia with images of soaring the Morning Glory.
- Cloud Appreciation Society Article on the Morning Glory, images, and video.
- Sable Island Green Horse Society Sable Island Soliton in the afternoon of 13 June 2003 – The same formation as a classic Gulf Morning Glory cloud
- Sable Island Green Horse Society More photos of the Sable Island Soliton