Rapid
warming of the ocean near Tasmania may provide a good indication of how the
water around New Zealand will change as the planet warms, say NIWA scientists
The following is a news release from National Institute of Water and Atmospheric Research (NIWA) in New Zealand.
In a recent paper, published in the New Zealand Journal of Marine and Freshwater Research, the scientists have used two Earth System Models and four climate change scenarios to project how New Zealand waters will be affected by 2100.
Lead author and NIWA marine biogeochemist Professor Cliff Law says the best-case scenario involved a cessation in the production of carbon dioxide in the next few years, with the worst-case being business as usual in which carbon dioxide levels keep rising.
“The average warming around New Zealand is 2.5°C by the end of this century, which will affect how the ocean mixes and the nutrients available for plankton growth, with knock-on effects on the foodweb and fisheries.”
Prof Law says that the surface ocean has a “density step” between the surface water and the lower, deeper water where the nutrients come from, which acts like a physical barrier to nutrient movement between the layers.
“With further warming, there’s a stronger density step and less nutrient supply for the surface waters so phytoplankton doesn’t grow so well and productivity drops down.” This has already happened in the water just off Tasmania and the south-east corner of Australia, which is warming rapidly as the East Australian current pushes warmer water further south causing huge changes to the ecosystem. There coastal ecosystems were changing with an increase in subtropical species, which can impact the economy, Prof Law said.
“We are predicted to get an equivalent amount of warming by the end of the century, so what’s happening to the ecosystem off Tasmania might be a good proxy for what we’re going to see in New Zealand waters.”
The paper reports that one of the most affected areas for nutrient decline will be the Chatham Rise to the east of New Zealand, which currently provides about 60 per cent of the country’s commercial fish catch. Another vulnerable area is the sub Antarctic waters to the south of New Zealand which is also home to some commercial fisheries.
The fishing industry may need to think about being more agile in terms of the species it catches and where it catches them, Prof Law said. “For example, if fish go deeper to maintain their temperature, they will have to adjust their practices to account for that.”
Acidity in the ocean will increase by 130 per cent by the end of the century which will cause changes to shellfish.
“For example, we can speculate that shells of paua and mussels may be affected – it doesn’t mean that we lose them from our ecosystems, just that they might become smaller in response to their diversion of energy to maintain their shells.”
Changes in species in New Zealand waters could include more invasive species and possibly new diseases that could affect local ecosystems. However, there may also be an upside. Tuna could be more plentiful in our waters because they prefer warmer waters and other fisheries may also benefit.
“In New Zealand we’re on the border between the warmer water, where things are moving from, and the cooler water, where things are moving to. Therefore, we won’t be as hard hit as some of the islands in tropical regions where continual warming will reduce numbers of fish and plankton.”
He also said the Earth Systems Models used by the scientists provided the best data “for now” but their global scale meant they provided information at low resolution.
“This paper is a first look at what these models suggest future conditions might be around New Zealand. But if we want more information we need to develop our own models that can give us more precision and greater resolution on a spatial scale.”
Prof Law said the aim of the paper was to inform the public and policy makers that conditions are going to change, “People tend to think of climate change from a terrestrial angle but obviously, as the ocean is a big part of the globe, there will be significant changes. As it’s also a significant part of New Zealand’s Exclusive Economic Zone we need to start planning for this now.”
Visit the NIWA website, HERE.
The following is a news release from National Institute of Water and Atmospheric Research (NIWA) in New Zealand.
In a recent paper, published in the New Zealand Journal of Marine and Freshwater Research, the scientists have used two Earth System Models and four climate change scenarios to project how New Zealand waters will be affected by 2100.
Lead author and NIWA marine biogeochemist Professor Cliff Law says the best-case scenario involved a cessation in the production of carbon dioxide in the next few years, with the worst-case being business as usual in which carbon dioxide levels keep rising.
“The average warming around New Zealand is 2.5°C by the end of this century, which will affect how the ocean mixes and the nutrients available for plankton growth, with knock-on effects on the foodweb and fisheries.”
Prof Law says that the surface ocean has a “density step” between the surface water and the lower, deeper water where the nutrients come from, which acts like a physical barrier to nutrient movement between the layers.
“With further warming, there’s a stronger density step and less nutrient supply for the surface waters so phytoplankton doesn’t grow so well and productivity drops down.” This has already happened in the water just off Tasmania and the south-east corner of Australia, which is warming rapidly as the East Australian current pushes warmer water further south causing huge changes to the ecosystem. There coastal ecosystems were changing with an increase in subtropical species, which can impact the economy, Prof Law said.
“We are predicted to get an equivalent amount of warming by the end of the century, so what’s happening to the ecosystem off Tasmania might be a good proxy for what we’re going to see in New Zealand waters.”
 |
| Projected
changes in upper ocean properties in response to climate Image credit: NIWA |
The paper reports that one of the most affected areas for nutrient decline will be the Chatham Rise to the east of New Zealand, which currently provides about 60 per cent of the country’s commercial fish catch. Another vulnerable area is the sub Antarctic waters to the south of New Zealand which is also home to some commercial fisheries.
The fishing industry may need to think about being more agile in terms of the species it catches and where it catches them, Prof Law said. “For example, if fish go deeper to maintain their temperature, they will have to adjust their practices to account for that.”
Acidity in the ocean will increase by 130 per cent by the end of the century which will cause changes to shellfish.
“For example, we can speculate that shells of paua and mussels may be affected – it doesn’t mean that we lose them from our ecosystems, just that they might become smaller in response to their diversion of energy to maintain their shells.”
Changes in species in New Zealand waters could include more invasive species and possibly new diseases that could affect local ecosystems. However, there may also be an upside. Tuna could be more plentiful in our waters because they prefer warmer waters and other fisheries may also benefit.
“In New Zealand we’re on the border between the warmer water, where things are moving from, and the cooler water, where things are moving to. Therefore, we won’t be as hard hit as some of the islands in tropical regions where continual warming will reduce numbers of fish and plankton.”
He also said the Earth Systems Models used by the scientists provided the best data “for now” but their global scale meant they provided information at low resolution.
“This paper is a first look at what these models suggest future conditions might be around New Zealand. But if we want more information we need to develop our own models that can give us more precision and greater resolution on a spatial scale.”
Prof Law said the aim of the paper was to inform the public and policy makers that conditions are going to change, “People tend to think of climate change from a terrestrial angle but obviously, as the ocean is a big part of the globe, there will be significant changes. As it’s also a significant part of New Zealand’s Exclusive Economic Zone we need to start planning for this now.”
Visit the NIWA website, HERE.
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