First of all – it’s good to be back. I apologize for the lengthy dry spell in my blogs, but it could not be helped (see blog post “Sorry-but there was an accident”, 6/29). I am glad to be back. And I am very glad that you are back reading my articles. I hope that my recovery will soon allow me to get back out to experience the joy of long hikes in the woods.
Recently, there have been numerous articles regrading Boaty McBoatface, and I want to salute the vessel, the drone, the scientists, and the findings.
First the vessel. You may remember in 2016 there was a public request by a British government bureau, the British Natural Environment Research Council (NERC), to submit names for a new scientific vessel. The vessel was a 425 foot (129 meter), $300 million ocean-going ice breaker and research vessel dedicated to the study of the oceans of the Antarctic regions.
I need to mention the importance of the protein provided by the oceans to the world’s population. According to the United Nations Food and Agriculture Organization (FAO), in 2014 “ten percent of the world’s population depends on fisheries for their livelihoods, and 4.3 billion people are reliant on fish for 15 percent of their animal protein intake.” [1] The oceans are an important resource and must be studied and protected.
The name for the vessel that the majority of people, those who visited the NERC website, recommended was Boaty McBoatface. I believe the world agreed it was a very funny, but a rather silly, name for a vessel of its size and importance.
The vessel, due to its expense and significance, was eventually named Royal Research Ship (RRS) David Attenborough after the famed broadcaster and natural historian. This name had also scored highly on the NERC website. But what then to do with that great and popular name of Boaty? The scientific community decided to use the name for a new and important drone vehicle. The new drone was planned for exploration of the oceans and specifically to collect data related to the temperature regions/levels of the ocean water surrounding Antarctica.
The new Boaty McBoatface submersible, is a research drone which can be launched and recovered from a larger research vessel. The submersible drone is a Autosub Long Range (ALR). Boaty McBoatface is the first of its class and is designated ALR-1. According to the NERC, the ALR submersibles can be at sea for weeks to months. This length of time and data gathering capability is far longer than research drones that are currently utilized by the NERC. Other autonomous vehicles of the Boaty class are planned for development, construction, and use for research of the Southern Ocean and perhaps others of the world’s seven seas.
ALR Boaty McBoatface, has been in the news recently for its data collection during its first scientific voyage. The data provides information regarding the effect of increasingly stronger winds on the rise of ocean surface water temperatures. This is one of the many feed-back loops related to global warming. According to an article published in the Proceedings of the National Academy of Science (PNAS) [2], ALR-1 (Boaty), traveled 112 miles on its first voyage. Its path took it through high walled underwater valleys of the Orkney Passage in the depths of the Southern Ocean near Antarctica. The vessel measured temperature, salinity (saltiness), as well as the turbulence at different depths.
The findings of Boaty’s maiden voyage reveal how increasingly stronger winds on the surface of the Southern Ocean create turbulence deep under the surface. This turbulence results in a mixing of the warm water at the middle levels with the colder waters from the depths of the Southern Ocean. This mixing causes the temperature of the waters in the lower level to warm and move upward through the water column. This can be a significant factor in rising sea levels. As the warmer water raises the overall ocean temperature, the water tends to expand due to the warming and thus causes the sea level to rise. If the deep-water warming contributes to a warming of the ocean’s surface waters this may increase the rate of evaporation from the surface into the atmosphere which can contribute to more rain and snow inland and greater strength to ocean storms.
According to the PNAS article, the significance of the findings of this previously undocumented mixing mechanism of the overturning circulation in the Southern Ocean is a better understanding that the deep-ocean waters are rapidly laundered through intensified near-boundary turbulence and boundary–interior exchange. As the conditions triggering this mechanism are common to other branches of the overturning circulation, the findings highlight a requirement for representing the newly-understood circulation in computer models of the overturning in the Southern Ocean and its effect of rising ocean water temperatures.
Congratulations to Boaty and the entire research team.
The artwork for this blog post is based on Figure 2 of the PNAS article (graph (D) showing the potential vorticity in red and blue and the neutral density of the deep water shown by the black contour lines). The image of the ALR-1 is taken from the internet.
[1] http://www.fao.org/news/story/en/item/248479/icode/, Oceans crucial for our climate, food and nutrition
[2] Rapid mixing and exchange of deep-ocean waters in an abyssal boundary current, PNAS first published June 18, 2019 https://doi.org/10.1073/pnas.1904087116