Tag Archives: ocean

Over 268,000 tonnes of ocean plastic – neglect it at our peril Updated for 2026





There are at least 268,000 tonnes of plastic floating around in the oceans, according to new research by a global team of scientists.

The world generates 288m tonnes of plastic worldwide each year – just a little more than the annual vegetable crop – yet using current methods only 0.1% of it is found at sea.

The new research illustrates as much as anything, how little we know about the fate of plastic waste in the ocean once we have thrown it ‘away’.

Where does it go? Into the food chain …

Most obviously, this discarded plastic exists as the unsightly debris we see washed ashore on our beaches.

These large chunks of plastic are bad news for sea creatures which aren’t used to them. Turtles, for instance, consume plastic bags, mistaking them for jellyfish.

In Hawaii’s outer islands the Laysan albatross feeds material skimmed from the sea surface to its chicks. Although adults can regurgitate ingested plastic, their chicks cannot. Young albatrosses are often found dead with stomachs full of bottle tops, lighters and other plastic debris, having starved to death.

But these big, visible impacts may just be the tip of the iceberg. Smaller plastic chunks less than 2.5mm across – broken down bits of larger debris – are ubiquitous in zooplankton samples from the eastern Pacific.

In some regions of the central Pacific there is now six times as much plankton-sized plastic are there is plankton. Plankton-eating birds, fish and whales have a tough time telling the two apart, often mistaking this plastic – especially tan coloured particles – for krill.

The smaller the pieces, the worse they get

However, even this doesn’t quite tell the whole story. For technical reasons Eriksen and his team weren’t able to consider the very smallest particles – but these may be the most harmful of all.

We’re talking here about tiny lumps of 0.5mm across or considerably less, usually invisible to the naked eye, which often originate in cosmetics or drugs containing nanoparticles or microbeads.

Such nanoparticles matter as they are similar size to the smallest forms of plankton (pico and nano plankton) which are the most abundant plankton group and biggest contributors in terms of biomass and contribution to primary production. There’s a lot going on when you zoom right in.

We don’t yet know precisely how plastic nanoparticles interact with marine fauna but we do know that they can be absorbed at the level of individual cells.

And what’s worse is they’re very efficient carriers of organic molecules such as estradiol, the drug used for birth control and IVF that finds it way through our sewage system into the sea.

Indeed, this efficiency is one of the reasons nanoparticles are being explored for drug delivery – they’re a great way to get the right medicine absorbed into the right cells.

Therefore it isn’t just the plastic itself that should concern us. We need to look at what it’s carrying, as substances clinging to nanoparticles of plastic could badly damage marine ecosystems.

A problem we neglect at our peril

Nasty endocrine disrupting chemicals can be concentrated a million times more than background levels on the surfaces of plastic particles. These can then be ingested by organisms and the chemicals absorbed leading to disruption of the reproductive process – some species such as bivalve mussels have even seen males turned into females.

Floating chunks of plastic can also be colonised by organisms including potential bacterial pathogens such as cholera, and marine insect sea skaters which need a hard surface to lay their eggs on – plastic in the sea increases their numbers and range.

The fact that floating plastic debris is novel and persists for longer than most natural flotsam could make them ideal vehicles for the introduction of invasive species with potentially devastating consequences.

Plastic pollution of the marine environment is the Cinderella of global issues, garnering less attention than its ugly sisters climate change, acidification, fisheries, invasive species or food waste but it has links to them all and merits greater attention by the scientific community.

 


 

Magnus Johnson is Senior Lecturer Environmental Marine Biology at the University of Hull.

Melanie Coull is a PhD researcher in Environmental Marine Biology at the University of Hull.

This article was originally published on The Conversation. Read the original article.

The Conversation

 




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Now is our chance to deliver on the 30% ocean protection target Updated for 2026





Top scientists, senior government managers, industry representatives, conservationists and even some nations’ presidents are currently in Sydney, Australia for the World Parks Congress.

This major international meeting happens only once a decade, and provides a critical opportunity to share the latest scientific knowledge and management of protected areas, both land-based and marine.

It is also a time for assessing progress and reviewing targets that drive the world’s conservation reserves.

The latter can be a bit tricky. The hosts of the congress include the New South Wales and Australian governments – both of which could until recently have claimed to be making great, if not world-leading, progress towards securing the necessary balance between what we take and what we conserve in our oceans.

But despite the best available science, both governments have recently chosen to reduce this progress to at best a standstill, in the case of the federal government’s decision to scrap previous plans for new reserves, and at worst a full about-face, with NSW allowing recreational fishing into existing ‘no-take’ marine parks.

The world is backsliding on marine park promises

Were this just an Australian phenomenon, it would be bad enough. But global progress towards achieving the marine target has been excruciatingly slow.

Currently, less than 3% of the world’s ocean is protected in marine parks, with only 1% afforded full protection in no-take sanctuaries. Is it any wonder that marine parks have yet to stem global declines in marine biodiversity?

The World Parks Congress provides a critical opportunity to reaffirm the global commitment to protecting at least 30% of the world’s oceans in highly protected marine parks.

A key outcome at the previous World Parks Congress, in Durban in 2003, was a pledge to place 20-30% of the world’s oceans in no-take marine sanctuaries. This target was set on the basis of a very clear recognition that healthy oceans are essential to human well being, and that healthy oceans need marine parks.

This is underpinned by decades of science that supports the design and establishment of marine parks and demonstrates their ecological benefits.

Not just ecology benefits, but economy

But since the Durban congress, further research, much of which is Australian-led, has shown that marine parks also deliver economic benefits. Here’s how:

  • Marine parks support commercial and recreational fishing. Researchers led by Hugo Harrison from James Cook University have shown that, across an area of some 1,000 sq km, the highly protected green zones of the Great Barrier Reef Marine Park exported 83% of young coral trout to fished reefs.
  • Marine parks reduce the cost of climate change by improving ecosystem resilience. Amanda Bates and colleagues have found that Tasmanian temperate reefs in marine parks are less likely to be invaded by tropical species than areas open to fishing, an important factor given the ability of tropical invaders to disrupt reef health.
  • Marine parks support ecosystem recovery in the face of environmental catastrophes. A study led by Andrew Olds found that coral reefs devastated by freshwater runoff in the 2011 Brisbane floods recovered more rapidly and more fully if they were inside the Great Barrier Reef’s no-take green zones, compared with those elsewhere in the Great Barrier Reef Marine Park.

Australia’s Centre for Policy Development has also published studies on the value of the ‘ecosystem services’ that Australia’s oceans provide us for free – such as nurseries for fish and opportunities for recreation.

In its report, former World Bank economist Caroline Hoisington calculated that the national network of marine protected areas proposed in 2012 could provide services worth A$1.2 billion a year, making a total of A$2 billion when added to Australia’s existing marine parks.

Building on success

We know what it takes to make a successful marine park. We need significant areas of full protection in no-take sanctuaries, because partial protection (that is, allowing some users into the area) does not work for conservation.

We need to invest adequately in enforcing them. And the marine parks need to be large, so that species are buffered from other ocean uses, and to ensure that wide-ranging species are protected.

Now is the time to build on the rising tide of marine park establishment. The United Kingdom protected the Chagos Islands in 2010, the United States recently announced protection for its Pacific Remote Islands, and Palau has announced its intention to close its waters to foreign fishing, and to allow limited domestic fishing only in certain small areas.

Returning to the opening irony of hosting the World Parks Congress in Sydney, Australia was a global leader by putting in place the world’s first national network of marine parks – right through the ocean territory that Australia manages – our Exclusive Economic Zone – the world’s third largest.

This global leadership is now at risk with the Australian Government having suspended the network pending a review, initiated despite more than 10 years of consultation and strong scientific support.

It’s time to be bold, both in Australia and globally. We need to undertake a step change in our approach to marine protection, reinforcing the target of effective protection for 30% of the world’s oceans as determined at the Durban congress more than a decade ago.

The science is clear. The benefits are well documented. Healthy oceans mean healthy economies, and healthy oceans mean marine parks.The Conversation

 


 

Jessica Meeuwig is Professor & Director, Centre for Marine Futures at University of Western Australia. She does not work for, consult to, own shares in or receive funding from any company or organisation that would benefit from this article, and has no relevant affiliations.

This article was originally published on The Conversation. Read the original article.

 




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A Marine Charter to protect and revitalise the UK’s ocean riches Updated for 2026





Five years ago to the day, the landmark Marine & Coastal Access Act 2009 was passed in the Westminster Parliament, enshrining in law a commitment to establish a network of Marine Protected Areas (MPAs) in English and Welsh inshore waters, and all offshore UK waters.

Successive Marine Acts passed in Holyrood and Stormont in 2010 and 2013 respectively required new MPAs in Scottish and Northern Irish inshore waters.

Each of these pieces of legislation committed to a broader goal – the creation of a network of MPAs throughout UK waters. The significance of this commitment was twofold.

Firstly, the commitment to a network of MPAs, rather than just cherry-picking areas in isolation, signalled the recognition of the need to take a more holistic view of the health of our oceans. This shift marked the UK’s ambition to become a global leader in restoring our increasingly denuded marine environment.

Secondly, the 2009 Marine Act was passed with overwhelming cross-party support. Members from across the benches acknowledged that the need to better protect and recover our iconic seas was not up for debate.

 How far have we got in five years?

We have undoubtedly made some headway. Following almost four years of consultation, in November 2013 the first 27 Marine Conservation Zones (MCZs – the formal name of English MPAs) were designated in inshore English waters and UK waters adjacent to England and Wales, with a commitment to two further tranches in 2015 and 2016.

In July 2014, the Scottish Government announced the designation of 30 Nature Conservation MPAs throughout waters adjacent to Scotland, with a further four to be consulted on in 2015. The Welsh Government has also committed to a review of existing MPAs within Welsh Inshore Waters.

But despite this, we remain a long way from the ambition of a full UK network. While welcome, the first 27 MCZs in the English MCZ project area were still 100 shy of the 127 originally proposed for that component of the UK network.

Crucially, it’s not enough just to declare MPAs. They also need to be properly managed and protected. Without this, the wafer thin veneer of progress is in reality leaving our seas with little more than paper parks. (See ‘Taking the ‘conservation’ out of Marine Conservation Zones‘.)

Not one of the 27 MCZs even has an agreed management plan in place. Throughout our seas, 35 marine species are still considered threatened by the International Union for Conservation of Nature (IUCN).

While the respective processes throughout the UK administrations are at different stages, the overall picture is one of a job half done – if that.

The Marine Charter for a comprehensive network of MPAs

So with the 2015 UK General Election looming, campaigners have sought to demonstrate that the strength of cross-party resolve that delivered the original 2009 Marine Act remains as strong as ever.

So far 21 UK NGOs – including the Marine Conservation Society, Wildlife Trusts, National Trust, RSPB and WWF – have united under the umbrella of Wildlife and Countryside Link to champion the Marine Charter – a call

“for the swift designation of a representative and well managed Ecologically Coherent Network of Marine Protected Areas in UK seas by 2016” that “meets international principles on coherence, and represents the full range of features in the UK seas as required by the relevant Marine Acts.

“The full network must include ambitious proposals within the commitment to two future tranches of Marine Conservation Zones in English Seas in 2015/16, alongside wider marine protected areas, and must be well managed to maintain sites that are in good condition and recover those that are damaged.

“Such a network is essential not only to stem the alarming decline in marine habitats and species, but also to ensure that the enormous social and economic benefits derived from marine goods and services can be realised for generations to come.”

Our aim – to secure commitments for the 2015 elections

The goal of the campaign is to secure commitments within the 2015 General Election Manifestos to complete a well-managed network of MPAs throughout UK seas by 2016.

As hoped, the Charter’s message has resonated across the parties. So far 127 MPs and 20 Peers from Labour, Liberal Democrats, SNP, Conservatives, DUP, SDLP, Greens and Plaid Cymru have all signed up in support.

In the last 18 months both the House of Commons Science & Technology and Environmental Audit Select Committees have urged the swift designation of the full list of 127 English MCZs toward the UK network.

Parallel advocacy is pushing for the completion of the respective parts of the network in Scotland, Wales and Northern Ireland. This strength of political, public and scientific support adds considerable weight to the enormous and diverse constituency who support a full network of MPAs in all UK waters.

The demand is also backed by more than 300,000 public signatures, 86 scientists from the UK’s marine biological community, and the Sea Users Development Group (SUDG), which represents a variety of maritime industries.

Certainty on exactly when these sites will be designated, says the SUDG, is vital for investor clarity and confidence

We need firm promises with no get-out clauses!

Secondly, and perhaps more significantly, the Charter represents unabashed and broad-based support for an issue that many may consider to have fallen down the political pecking order – conservation.

Here is clear recognition that this network is about far more than obscure bits of seaweed – it’s about better managing the very building blocks of the ecosystems that we have for too long taken for granted.

Yet, we are all, sadly, aware of how fickle political commitments can be. Hence it is crucial that rhetoric translates into firm commitments, underpinned by the political will to drive and coordinate the widely shared ambition to conserve and revitalise our marine heritage.

We all – politicians included – rightly take great pride in and evoke our island nation status.

It is not difficult to hark back to the majesty of our seas. A hundred years ago vast native oyster fields the size of Wales carpeted the Irish Sea; thriving coastal communities such as Lowestoft, Great Yarmouth and Grimsby harboured great fleets of vessels in their pursuit of the vast herring schools throughout the North Sea; and stunning apex predators such a Bluefin Tuna, Common Skate and Angel Sharks were abundant.

Sadly, we still have much to do to restore these former glories – and we must be candid that our ability to take great pride in our seas now comes with the responsibility of good stewardship.

Politicians from across Westminster have signalled their continued support to finish the job, but at a time when trust in our politicians and institutions have never been under greater scrutiny, the real test is whether this supports translates into the leadership that is so necessary.

 


 

Tom Hickey is Policy and Parliamentary Officer at the Marine Conservation Society.

 




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New wave generator brightens ocean power prospects Updated for 2026





Generating electricity from the waves in Britain took a step closer to reality this week after an innovative device – Searaser – successfully completed its first stage testing.

A 1:14 scale model of the device went through exhaustive tests at Plymouth University’s CoastLAB wave tank to verify its computed outputs in Britain’s coastal waters, and to ensure its sturdiness under extreme sea conditions.

The brainchild of British inventor Alvin Smith, Searaser is designed to overcome two of the biggest hurdles in the deployment of renewable energy on a scale that fulfils Britain’s future electricity needs – cost and variable output.

Green energy company Ecotricity and the Searaser team have spent the past 18 months optimising the design of the device and modelling outputs in real word conditions around the coast of Britain – with the assistance of marine energy consultants DNV GL Group.

Resilience to extreme conditions is essential

The determining factor in making wave power viable is resilience to often violent sea conditions, said Smith: “We’ve put Searaser through the most extreme testing regime here at CoastLAB and it’s passed every challenge.”

“This week’s wave tank testing was carried out to validate the extensive computer modelling we’ve been undertaking”, he added.

Unlike other marine energy technologies, Searaser won’t generate electricity out at sea but will simply use the motion of the ocean swell to pump high pressure seawater ashore, where it will be used to make electricity.

The motion of the waves drives a piston between two buoys – one on the surface of the water, the other suspended underwater and tethered to a weight on the seabed.

As waves move past, the surface buoy moves the piston up-and-down, pumping volumes of pressurised seawater through a pipe to an onshore hydropower turbine to produce electricity.

The Searaser could also be used to pump seawater into coastal reservoirs elevated well above sea level. The stored water could then be released at any time of the day or night to make renewable electricity on demand.

The sea could produce a significant proportion of the UK’s power

Ecotricity founder Dale Vince said: “Our vision is for Britain’s electricity needs to be met entirely from our big three renewable energy sources – the wind, the sun and the sea.

“Out of these three energy sources, generating electricity from the sea is by far the most difficult due to the hostile ocean environment – it’s also the least advanced of the three technologies but it has enormous potential.

“We believe these ‘Seamills’ have the potential to produce a significant amount of the electricity that Britain needs, from a clean indigenous source and in a more controllable manner than currently possible.”

Ecotricity hopes to have a full scale prototype in the ocean in the next 12 months or so, measuring some 12m deep and 1m wide. A first commercial array of ‘Searasers’ could be producing electricity within a few years. Each device will be rated at 1.5 MW electrical capacity – similar to a large wind turbine.

“The potential is enormous”, said Dale. “This is a British invention that could transform the energy market not just here in Britain but around the world. Our plan is to develop the technology and make them here in Britain, bringing green jobs as well as green energy to our country.”

Ecotricity now powers almost 150,000 homes and businesses from a growing fleet of wind and sun parks. The company prides itself on building more green electricity generation capacity than any other energy company in Britain.

 

 




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Ocean acidification and greenhouse gases hit new records Updated for 2026





The World Meteorological Organisation (WMO) has reported that the amounts of atmospheric greenhouse gases reached a new high in 2013, driven by rapidly rising levels of carbon dioxide.

The news is consistent with trends in fossil fuel consumption. But what comes as more of a surprise is the WMO’s revelation that the current rate of ocean acidification, which greenhouse gases (GHGs) help to cause, appears unprecedented in at least the last 300 million years.

“We know without any doubt that our climate is changing and our weather is becoming more extreme due to human activities such as the burning of fossil fuels”, said the WMO’s secretary-general, Michel Jarraud.

“The Greenhouse Gas Bulletin shows that, far from falling, the concentration of carbon dioxide in the atmosphere actually increased last year at the fastest rate for nearly 30 years. We are running out of time. The laws of physics are non-negotiable.

A 34% increase in radiative forcing from 1990 – 2013

The details of growing GHG levels are in the annual Greenhouse Gas Bulletin, published by the WMO – the United Nations specialist agency that plays a leading role in international efforts to monitor and protect the environment.

The Bulletin reports on atmospheric concentrations – not emissions – of greenhouse gases. Emissions are what go into the atmosphere, while concentrations are what stay there after the complex system of interactions between the atmosphere, biosphere (the entire global ecological system) and the oceans.

The Bulletin shows that between 1990 and 2013 there was a 34% increase in radiative forcing – the warming effect on our climate – because of long-lived greenhouse gases such as carbon dioxide (CO2), methane and nitrous oxide.

About a quarter of total emissions are taken up by the oceans and another quarter by the biosphere, cutting levels of atmospheric CO2.

In 2013, the atmospheric concentration of CO2 was 142% higher than before the Industrial Revolution started, in about 1750. Concentrations of methane and nitrous oxide had risen by 253% and 121% respectively.

Reduced CO2 absorption by the biosphere?

The observations from WMO’s Global Atmosphere Watch network showed that CO2 levels increased more from 2012 to 2013 than during any other year since 1984. Scientists think this may be related to reduced CO2 absorption by the Earth’s biosphere, as well as by the steady increase in emissions.

Although the oceans lessen the increase in CO2 that would otherwise happen in the atmosphere, they do so at a price to marine life and to fishing communities – and also to tourism. The Bulletin says the oceans appear to be acidifying faster than at any time in at least the last 300 million years.

Wendy Watson-Wright, executive secretary of the Intergovernmental Oceanographic Commission of UNESCO, said: “It is high time the ocean, as the primary driver of the planet’s climate and attenuator of climate change, becomes a central part of climate change discussions.

“If global warming is not a strong enough reason to cut CO2 emissions, ocean acidification should be, since its effects are already being felt and will increase for many decades to come.”

The amount of CO2 in the atmosphere reached 396.0 parts per million (ppm) in 2013. At the current rate of increase, the global annual average concentration is set to cross the symbolic 400 ppm threshold within the next two years.

Other potent greenouse gases

Methane, in the short term, is a far more powerful greenhouse gas than CO2 – 34 times more potent over a century, but 84 times more over 20 years.

Atmospheric methane reached a new high of about 1,824 parts per billion (ppb) in 2013, because of increased emissions from human sources. Since 2007, it has started increasing again, after a temporary period of levelling-off.

Nitrous oxide’s atmospheric concentration in 2013 was about 325.9 ppb. Its impact on climate, over a century, is 298 times greater than equal emissions of CO2. It also plays an important role in the destruction of the ozone layer that protects the Earth from harmful ultraviolet solar radiation.

The oceans currently absorb a quarter of anthropogenic CO2 emissions – about 4kg of CO2per day per person. Acidification will continue to accelerate at least until mid-century, according to projections from Earth system models.

“The Bulletin provides a scientific base for decision-making”, concluded Jarraud. “We have the knowledge and we have the tools for action to try to keep temperature increases within 2°C to give our planet a chance and to give our children and grandchildren a future. Pleading ignorance can no longer be an excuse for not acting.”

 


 

Alex Kirby writes for Climate News Network.

 

 




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Heat accumulating in the deep oceans has put global warming on pause Updated for 2026





There seem to have been a dozen or so explanations for why the Earth’s surface has warmed at a slower rate over the past 15 years compared to earlier decades.

This is perhaps not so surprising given the complexity of the climate system – the world’s best detectives will inevitably struggle to disentangle the factors which influence every lump and bump in the surface temperature record.

However, recent research implicates natural changes in the Pacific and Atlantic oceans as the prime culprits. Just as the apparently random motions in a river’s flow can shift before our eyes from one minute to the next, the gradual sloshing about of our vast ocean waters can influence Earth’s climate from one year to the next and from one decade to the next.

Natural variability and long term trends

It is clear that natural variability has and always will influence the climate. In addition to chaotic ocean fluctuations, changes in the brightness of the sun and variations in the frequency and intensity of volcanic eruptions (which cool the planet temporarily with sunlight-reflecting aerosol particles) influence the surface temperature.

The recent Intergovernmental Panel on Climate Change working report found that these natural factors have contributed toward the slowing rate of surface warming since 1998.

However, recent measurements of ocean temperature made by thousands of automated buoys and observations of Earth’s radiative energy budget by satellite instruments indicate that heating has continued at a rate equivalent to every person worldwide using about 20 kettles each to continuously boil the oceans.

This is consistent with what is expected from the rising atmospheric concentrations of greenhouse gases due to human activity. If anything, Earth’s heating rate increased between the 1985-1999 and 2000-2012 periods, despite a slowing in the rate of surface warming.

In search of the hidden heat – the Pacific?

So, how is it possible for increased heating to not directly correspond with surface warming?

The Earth’s heating is caused by an imbalance between the amount of absorbed sunlight and the heat emitted back to space. This surplus of heat is primarily absorbed by the oceans since they command the lion’s share of storage capacity compared with other parts of the climate system such as the land, the atmosphere or the cryosphere (ice and snow).

This large heat capacity of water is noticeable from the amount of time it takes to heat up your pan of vegetables. And there is a lot of water in the oceans – nearly a fifth of a cubic kilometre of water for each person on the planet.

Crucially, the temperature at the Earth’s surface depends upon where this heat is deposited in the oceans. If the upper levels warm, so too will the atmosphere above. However, if ocean circulations cause more heat to be drawn down to deeper depths (or less heat to be moved upward toward the sea surface) then surface temperatures will reflect this.

Recent research has implicated our largest ocean, the Pacific, as the most likely mechanism for subducting heat to deeper levels. Indeed, atmospheric and ocean conditions in the Pacific have been unusual in the past decade and computer simulations show that decades of slow surface warming despite rising greenhouse gas concentrations are associated with increased heating below 300m depth.

The mechanisms for heat absorption are less clear; the simulations show that similar patterns appearing to originate from the Pacific are associated with the draw-down of heat in the North Atlantic and Southern Ocean as well as the Pacific.

Or is it the Atlantic?

New research published in Science now shifts the focus towards the Atlantic Ocean. Xianyao Chen and Ka-Kit Tung of the University of Washington show that heating from rising greenhouse gas concentrations has preferentially warmed the ocean’s 300-1,500m layer since about 2000, thereby depriving the upper layers of this surplus heat and causing surface warming to slow.

The authors say these changes are part of a natural cycle of knock-on effects, involving ocean circulation responses to changes in how salty (and therefore dense) the upper Atlantic Ocean layers are.

This cycle is thought to last around 30 years, contributing a sustained cooling effect then a warming influence on surface temperatures. When combined with steady heating from greenhouse gas increases this leads to a ‘staircase’ effect of stable temperatures followed by rapid warming.

They argue the previous focus on the Pacific was based upon simulations that were unable to fully capture the intricacies of the Atlantic Ocean circulation. An observed decline in the North Atlantic Ocean circulation over recent years has also been identified as part of a longer-term shift based upon evidence from computer simulations.

Climate complexity disallows simple answers

The changes in ocean circulation have also been shown to influence seasonal extremes and, based upon the proposed Atlantic mechanism, may persist for another decade before rapid warming is re-established. However, the nature of internal ocean fluctuations means it is difficult to pin down timings with any confidence.

While it is human nature to seek a single cause for notable events, in reality the complexity of the climate system means that it is unlikely there is one simple reason for any extreme weather event or a decade of unusual climatic conditions.

Nevertheless, the recent hiatus in global surface warming has encouraged scientists to further scrutinise and learn in even finer detail than before the workings of our climate system.

 


 

Richard Allan is Professor of Climate Science at the University of Reading. He receives funding from the Natural Environment Research Council.

This article was originally published on The Conversation. Read the original article.

The Conversation

 




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