As an explorer of the water world, there is nothing I love more than finding a beautiful lake and going for a swim or a dive. I’ll picnic by the water and revel in the discovery of a sweet berry patch on a warm summer day. Wild blueberries contain the energy of the sun. They make me feel powerful. Here in this Treaty 11 Territory of Canada, the traditional territory of the Akaitcho and Tlicho Agreement People, the Native Dene describe at least 10,000 years of history. Their connection to the land is undeniable. On first inspection, this place looks…
Sponsored by the Royal Canadian Geographical Society, the Arctic on the Edge/L’Arctique à la limite Expedition documents the life cycle of ice from Greenland to Baffin Island, south down the Labrador Coast, ending in Newfoundland.
The polar region is warming more than twice as fast as the rest of the planet. That means that our northern geography is changing faster than anywhere else on earth. The scientific journal Nature reported in April 2017 that the Arctic is 3°C warmer now than baseline data from 1971 to 2000. The evidence is clear. The Arctic is undergoing a massive transformation at a time when we have barely documented what lies at the interface between the sea rapidly depleting ice. Arctic on the Edge will take a close look at the journey of sea ice and how it is transforming humanity and the natural world.
The story of sea ice begins in Greenland where glacial deposits meet calving grounds along the coast. In sheltered inlets, bays and fjords, glaciers march towards the ocean and break off into the sea. From there, they begin a voyage across the Davis Strait to Baffin Island and then, after a winter of sojourn, they continue south along the Labrador Coast to Newfoundland. In early 2017, reports indicate that ice conditions between Newfoundland and southern Labrador were the worst in recorded history hampering shipping and fishermen from their normal routes.
The Canadian Ice Service reported above normal ice melt in 2016, generally occurring 1-2 weeks ahead of normal across most of the Canadian Arctic, with some regions remaining 2-3 weeks ahead through the summer. By early September, ice cover was the third-lowest on record, behind 2012 and 2011. With changing ice conditions comes a change in the way of life for people and wildlife in the Arctic.
In March 2017, Jill Heinerth was presented with the Polar Medal by the Governor General of Canada at a ceremony in London, Ontario. The Polar Medal celebrates Canada’s northern heritage and recognizes persons who render extraordinary services in the polar regions and in Canada’s North. As an official honour created by the Crown, the Polar Medal is part of the Canadian Honours System.
READ: Last Ice in DIVER Magazine Diving the transitional environments of Bylot Island by Jill Heinerth
Making documentary films while immersed in the hostile, yet stunning waters of the Canadian Arctic, I need great technology to keep me warm and safe. The travel, dives, and image making all create their own set of unique challenges, and once you are in the north, there is no way to call up a dive shop for something you may have forgotten. I’ve spent many months in the polar region, most recently helping to create a film about climate change. Camping on the sea ice and then on a remote island outpost, I swam with polar bears, hovered below fighting…
I learned a new term for my climate change vocabulary today. Atlantification. This important article from CarbonTimes explains how the Arctic ecosystem is rapidly changing.
Dive Nunavut As I try to sleep on a cot in a tent on the sea ice in Lancaster Sound, Nunavut, I am surrounded by water. The water has seeped through the seams of the floor, and even though I am pitched on top of plywood sheets, the water is getting too deep. It is time to find slightly higher ground or a remnant snow drift that has not yet melted. It is the beginning of June, and the rain is pouring down. The closest community is Arctic Bay some 80 km away. Arctic Bay is an amazing, traditional community…
People often ask how long it takes me to prepare for a project. In some ways, I have made a lifetime of preparations for each endeavor that I embark upon. This time I am headed back to the northern reaches of my home country to shoot a story about climate change for a documentary film called “Under Thin Ice.” It will air on the esteemed program “Nature of Things,” in Canada and on media outlets around the world. It is an ambitious project that has been in pre-production for more than two years. This week I am handling the last…
MAPS: A GLOBAL PEACE SANCTUARY During a hot summer that felt as though the Earth itself was feverish, a Canadian singer named Parvati had a recurring dream in which she lay on a frozen ocean, while a great blue whale awaited her below. Though she was planning a musical tour of Asia, the dream was too vivid to ignore. Trusting the inner call, she canceled her tour and traveled to the North Pole where she performed to raise awareness of the melting polar ice. Having met in the Arctic with city councils, schools, hunters, scientists and elders, Parvati returned with…
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Climate Regulation
Ocean currents transport warm water and precipitation from the equator to the poles and cold water from the poles back to the tropics on a global conveyor system that regulates the world’s climate.
Deep Ocean Circulation
Deep-ocean currents and atmospheric circulation work together to transport massive amounts of heat and salt around the globe. Sunlight warmed water at the equator flows into the North Atlantic, where it is cooled and becomes saltier through evaporation. Cold, salty water is heavy and drops to the seafloor forming a massive undersea river. The deep water flows through the world’s oceans on a current-driven conveyor, rising in places where winds sweep away warm surface water. Freshwater evaporated from the Atlantic falls as rain on the Pacific, diluting the upwelling salty water with freshwater and restoring balance.
Surface Ocean Currents
The wind drives surface currents and in turn, influences atmospheric circulation. Both ocean and atmospheric circulation are shaped by the spin of the Earth. Surface currents form massive circular patterns called gyres that, because of the Earth’s rotation, flow clockwise in the northern hemisphere and counterclockwise in the Southern Hemisphere. Currents, on the edges of the gyres, carry warm tropical water to higher latitudes and cold polar water to the lower latitudes.
Loss of Sea Ice
NASA’s cryospheric scientist Dr. Walt Meier narrates this important visual. documenting changes in Arctic sea ice between 1984 and 2016. An updated version of this visualization can be downloaded in HD here.
The Problem
Global ice cover has been deteriorating for a long time. Over 50,000 years ago, the world’s ice sheets were so large that they held enough water to lower the world’s water level almost 400 feet. But around 25,000 thousand years ago, the ice sheets started melting, and shorelines slowly receded inland by as much as one hundred miles. Some of those remarkable ice sheets are still melting today at an ever accelerating rate, and the fate of ice sheets in Greenland and Antarctica will dictate the future geography of our planet.
The population of the planet is nearing 8 billion with hundreds of millions of people living on coastlines that provide real estate and resources, all within a few feet of current sea levels.