Learn how climate change affects the coral reefs
Learn how climate change affects the coral reefs
Overview of the effects of global warming on coral, including those off the coast of Tahiti.
Contunico © ZDF Studios GmbH, Mainz
Transcript
NARRATOR: Papeete on the island of Tahiti - diver Joël Orempuller is preparing for his next underwater investigation. No one knows the coral off the coast of Tahiti better than him. This lagoon is a second home to him - and he's worried about it. Slowly but surely, the reef is changing. Experts like Joël warn that this could have dire consequences. Joël has dived down to the reef over 3,000 times to photograph the coral and record his findings. It's very clear to him that climate change is already having an impact on these sensitive organisms. Constantly changing currents and water temperatures are forcing them to keep adapting. Coral live in shallow waters that are suffused with light. If the sea level rises, then the lack of sunlight could cause the coral to die, and that would have drastic consequences for the reef.
JOËL OREMPULLER: "Coral are extremely sensitive. A temperature difference of just two or three degrees is enough to put them in danger."
NARRATOR: Climatologists here at Bremen University's Marum Center for Marine Environmental Sciences are particularly interested in the last dramatic instance of global warming. They've developed computer simulations to discover just what happened at the end of the last ice age. Analyses of coral that died at the time will play a crucial role in their investigations. They aim to find out how quickly sea levels rose, and by how much. The vast quantities of ice that melted within a few hundred years must have had a dramatic impact on sea levels. But why did the ice melt? One clue seems to be in the ocean currents. Streams of warm water from tropical seas carry heat to high latitudes. One well-known example is the Gulf Stream. Researchers believe that huge ice masses in the northern hemisphere melted, releasing fresh water that flowed into the North Atlantic, reducing the density of the sea water and effectively switching off the Gulf Stream. So places in the northern hemisphere should actually have got colder. And it's this that's bothering scientists because their data suggest precisely the opposite. It didn't get colder, it got warmer. They're viewing an event from 20,000 years ago.
PROF. MICHAEL SCHULZ: "The transition from the last maximum glaciation to the warmer period we are currently experiencing gives us a perfect example of how ice sheets melt. And the better we can reconstruct what happened back then and manage to incorporate that into our simulations, then the more faith we can have in the ability of these simulations to show us how ice sheets might behave in the future."
NARRATOR: The key to the mystery is thought to lie in Tahiti. Scientists believe that samples of coral, extracted far away from the ice masses in the north, can help give them a precise picture of how and when sea levels rose the last time the Earth heated up. The reefs can be thought of as the memory banks of the ocean. If we can unlock their secrets, we'll be able to find out what effect the last great climate change had on our planet. The more exact the reconstruction, the more precisely we'll be able to predict the future of the reefs, and that of the Earth's oceans.
JOËL OREMPULLER: "Coral are extremely sensitive. A temperature difference of just two or three degrees is enough to put them in danger."
NARRATOR: Climatologists here at Bremen University's Marum Center for Marine Environmental Sciences are particularly interested in the last dramatic instance of global warming. They've developed computer simulations to discover just what happened at the end of the last ice age. Analyses of coral that died at the time will play a crucial role in their investigations. They aim to find out how quickly sea levels rose, and by how much. The vast quantities of ice that melted within a few hundred years must have had a dramatic impact on sea levels. But why did the ice melt? One clue seems to be in the ocean currents. Streams of warm water from tropical seas carry heat to high latitudes. One well-known example is the Gulf Stream. Researchers believe that huge ice masses in the northern hemisphere melted, releasing fresh water that flowed into the North Atlantic, reducing the density of the sea water and effectively switching off the Gulf Stream. So places in the northern hemisphere should actually have got colder. And it's this that's bothering scientists because their data suggest precisely the opposite. It didn't get colder, it got warmer. They're viewing an event from 20,000 years ago.
PROF. MICHAEL SCHULZ: "The transition from the last maximum glaciation to the warmer period we are currently experiencing gives us a perfect example of how ice sheets melt. And the better we can reconstruct what happened back then and manage to incorporate that into our simulations, then the more faith we can have in the ability of these simulations to show us how ice sheets might behave in the future."
NARRATOR: The key to the mystery is thought to lie in Tahiti. Scientists believe that samples of coral, extracted far away from the ice masses in the north, can help give them a precise picture of how and when sea levels rose the last time the Earth heated up. The reefs can be thought of as the memory banks of the ocean. If we can unlock their secrets, we'll be able to find out what effect the last great climate change had on our planet. The more exact the reconstruction, the more precisely we'll be able to predict the future of the reefs, and that of the Earth's oceans.