Friday, 11 October 2024
State of the Climate 2024 Report - continuing inconvenient truths abound
Wednesday, 9 October 2024
No improvement in climate change measurements
Unprecedented peril: disaster lies ahead as we track towards 2.7°C of warming this century
You don’t have to look far to see what climate change is doing to the planet. The word “unprecedented” is everywhere this year.
We are seeing unprecedented rapidly intensifying tropical storms such as Hurricane Helene in the eastern United States and Super Typhoon Yagi in Vietnam. Unprecedented fires in Canada have destroyed towns. Unprecedented drought in Brazil has dried out enormous rivers and left swathes of empty river beds. At least 1,300 pilgrims died during this year’s Hajj in Mecca as temperatures passed 50°C.
Unfortunately, we are headed for far worse. The new 2024 State of the Climate report, produced by our team of international scientists, is yet another stark warning about the intensifying climate crisis. Even if governments meet their emissions goals, the world may hit 2.7°C of warming – nearly double the Paris Agreement goal of holding climate change to 1.5°C. Each year, we track 35 of the Earth’s vital signs, from sea ice extent to forests. This year, 25 are now at record levels, all trending in the wrong directions.
Humans are not used to these conditions. Human civilisation emerged over the last 10,000 years under benign conditions – not too hot, not too cold. But this liveable climate is now at risk. In your grandchild’s lifetime, climatic conditions will be more threatening than anything our prehistoric relatives would have faced.
Our report shows a continued rise in fossil fuel emissions, which remain at an all-time high. Despite years of warnings from scientists, fossil fuel consumption has actually increased, pushing the planet toward dangerous levels of warming. While wind and solar have grown rapidly, fossil fuel use is 14 times greater.
This year is also tracking for the hottest year on record, with global daily mean temperatures at record levels for nearly half of 2023 and much of 2024.
Next month, world leaders and diplomats will gather in Azerbaijan for the annual United Nations climate talks, COP 29. Leaders will have to redouble their efforts. Without much stronger policies, climate change will keep worsening, bringing with it more frequent and more extreme weather.
Bad news after bad news
We have still not solved the central problem: the routine burning of fossil fuels. Atmospheric concentrations of greenhouse gases – particularly methane and carbon dioxide – are still rising. Last September, carbon dioxide levels in the atmosphere hit 418 parts per million (ppm). This September, they crossed 422 ppm. Methane, a highly potent greenhouse gas, has been increasing at an alarming rate despite global pledges to tackle it.
Compounding the problem is the recent decline in atmospheric aerosols from efforts to cut pollution. These small particles suspended in the air come from both natural and human processes, and have helped cool the planet. Without this cooling effect, the pace of global warming may accelerate. We don’t know for sure because aerosol properties are not yet measured well enough.
Other environmental issues are now feeding into climate change. Deforestation in critical areas such as the Amazon is reducing the planet’s capacity to absorb carbon naturally, driving additional warming. This creates a feedback loop, where warming causes trees to die which in turn amplifies global temperatures.
Loss of sea ice is another. As sea ice melts or fails to form, dark seawater is exposed. Ice reflects sunlight but seawater absorbs it. Scaled up, this changes the Earth’s albedo (how reflective the surface is) and accelerates warming further.
In coming decades, sea level rise will pose a growing threat to coastal communities, putting millions of people at risk of displacement.
Accelerate the solutions
Our report stresses the need for an immediate and comprehensive end to the routine use of fossil fuels.
It calls for a global carbon price, set high enough to drive down emissions, particularly from high-emitting wealthy countries.
Introducing effective policies to slash methane emissions is crucial, given methane’s high potency but short atmospheric lifetime. Rapidly cutting methane could slow the rate of warming in the short term.
Natural climate solutions such as reforestation and soil restoration should be rolled out to increase how much carbon is stored in wood and soil. These efforts must be accompanied by protective measures in wildfire and drought prone areas. There’s no point planting forests if they will burn.
Governments should introduce stricter land-use policies to slow down rates of land clearing and increase investment in forest management to cut the risk of large, devastating fires and encourage sustainable land use.
We cannot overlook climate justice. Less wealthy nations contribute least to global emissions but are often the worst affected by climate disasters.
Wealthier nations must provide financial and technical support to help these countries adapt to climate change while cutting emissions. This could include investing in renewable energy, improving infrastructure and funding disaster preparedness programs.
Internationally, our report urges stronger commitments from world leaders. Current global policies are insufficient to limit warming to 1.5°C above pre-industrial levels.
Without drastic changes, the world is on track for approximately 2.7°C of warming this century. To avoid catastrophic tipping points, nations must strengthen their climate pledges, reduce dependence on fossil fuels, and accelerate the transition to renewable energy.
Immediate, transformative policy changes are now necessary if we are to avoid the worst effects of climate change.
Climate change is already here. But it could get much, much worse. By slashing emissions, boosting natural climate solutions and working towards climate justice, the global community can still fend off the worst version of our future.
Thomas Newsome, Associate Professor in Global Ecology, University of Sydney and William Ripple, Distinguished Professor and Director, Trophic Cascades Program, Oregon State University
This article is republished from The Conversation under a Creative Commons license. Read the original article.
Thursday, 27 June 2024
Coral reefs in jeopardy
Devastating coral bleaching will be more common, start earlier and last longer unless we cut emissions
Coral bleaching is becoming much more common as a result of increasingly severe and frequent marine heatwaves. Four global mass bleaching events have happened since 1998. Two of these were in the past decade.
Unless greenhouse gas emissions are cut to slow global warming, our new research shows that, by 2080, coral bleaching will start in spring, rather than late summer. Some events will last into autumn. The Great Barrier Reef’s maximum annual heat stress will double by 2050 if emissions do not slow.
Marine heatwaves stress corals, which then expel the symbiotic algae living in their tissue. These corals are left white and weakened. While not all bleached corals die immediately, prolonged heat stress harms their health and reproduction.
Our research used daily data on sea surface temperatures (instead of monthly data that models typically use) and supercomputing to produce high-resolution projections of marine heatwaves. We showed the risk of coral bleaching will be greatest along the equator. That’s also where the most biodiverse coral reefs are found.
Coral reefs cover only 1% of our oceans, but host at least 25% of all marine species. More than half a billion people worldwide depend on coral reefs for food.
So coral reefs are vital for the health of the ocean and people. They are also among the ecosystems most at risk from climate change.
Longer bleaching season will hit spawning
The US National Oceanic and Atmospheric Administration monitors marine heatwaves globally. Seasonal coral bleaching alerts are based on this data. Predicting coral bleaching risk over entire decades has proved much more challenging.
Recent improvements in climate modelling now allow marine heatwaves and coral bleaching risks to be predicted with high accuracy. Using daily projections of heat stress from many global climate models, we show the severity and duration of coral bleaching will soon reach uncharted territory.
By mid-century coral bleaching is expected to start in spring for most of Earth’s reefs, rather than late summer as is typical today. In equatorial regions, corals will be at high risk of bleaching all year round by the end of the century.
In many regions, corals spawn only once a year. These spectacular mass spawning events happen in a single week following a full moon in spring.
By 2040, this spawning event could coincide with severe bleaching risk. This would greatly reduce their reproductive success, causing large-scale coral loss.
Equatorial regions most at risk
We show the future risk of severe coral bleaching is uneven globally.
The greatest risk is along the equator. Equatorial regions are home to the most biodiverse coral reefs, including conservation hotspots such as the Coral Triangle. To make matters worse, marine life in these regions is particularly vulnerable to accelerated climate change.
Many equatorial species are already living at temperatures near their upper tolerance. They also generally have low abilities to move to track shifting climates. This leaves them at high risk of extinction.
Our research shows equatorial regions are set to benefit least from efforts to curb emissions. We expect significant emission cuts will reduce the annual duration of severe bleaching conditions in all areas except these regions.
The projected highest climate impacts coincide with highest social reliance on coral reefs. This will challenge human populations that rely heavily on their local reefs for their livelihoods and nutrition.
Improving coral reef management
Our research identifies Earth’s reef regions that are at lowest risk of increased bleaching. This will help conservation managers and policymakers prioritise efforts to limit loss of coral reef biodiversity.
We predict much less risk of coral bleaching in regions such as the northern coasts of Venezuela and Colombia, Socotra Island (opposite the Gulf of Aden) and Alor Kecil in Indonesia. Seasonal upwellings occur here, bringing cooler water to the surface that’s likely to limit the severity of heatwaves.
Identifying these future havens for coral reefs will help maximise the success of coral conservation strategies such as assisted evolution, coral restoration or transplantation.
These strategies can help maintain healthy coral populations at local scales, particularly if used on reefs where future climate impacts will be lower. By pinpointing these havens, our research will strengthen coral conservation.
Our research includes a user-friendly web-based tool for mapping future coral bleaching. It will help pinpoint locations for effective management interventions.
Curbing greenhouse gas emissions is the main solution to reduce future climate impacts on corals. However, other strategies are also vital to maximise coral reefs’ adaptation to climate change.
Camille Mellin, Senior Lecturer and ARC Future Fellow, School of Biological Sciences, University of Adelaide and Damien Fordham, Associate Professor of Global Change Ecology, University of Adelaide
This article is republished from The Conversation under a Creative Commons license. Read the original article.
Friday, 9 February 2024
Has the world crossed the 1.5C warming threshold already ?
Shutterstock |
Tuesday, 16 January 2024
The warming of Antarctica
A heatwave in Antarctica totally blew the minds of scientists. They set out to decipher it – and here are the results
Dana M Bergstrom, University of WollongongClimate scientists don’t like surprises. It means our deep understanding of how the climate works isn’t quite as complete as we need. But unfortunately, as climate change worsens, surprises and unprecedented events keep happening.
In March 2022, Antarctica experienced an extraordinary heatwave. Large swathes of East Antarctica experienced temperatures up to 40°C (72°F) above normal, shattering temperature records. It was the most intense heatwave ever recorded anywhere in the world.
So shocking and rare was the event, it blew the minds of the Antarctic climate science community. A major global research project was launched to unravel the reasons behind it and the damage it caused. A team of 54 researchers, including me, delved into the intricacies of the phenomenon. The team was led by Swiss climatologist Jonathan Wille, and involved experts from 14 countries. The collaboration resulted in two groundbreaking papers published today.
The results are alarming. But they provide scientists a deeper understanding of the links between the tropics and Antarctica – and give the global community a chance to prepare for what a warmer world may bring.
Head-hurting complexity
The papers tell a complex story that began half a world away from Antarctica. Under La Niña conditions, tropical heat near Indonesia poured into the skies above the Indian Ocean. At the same time, repeated weather troughs pulsing eastwards were generating from southern Africa. These factors combined into a late, Indian Ocean tropical cyclone season.
Between late February and late March 2022, 12 tropical storms had brewed. Five storms revved up to become tropical cyclones, and heat and moisture from some of these cyclones mashed together. A meandering jet stream picked up this air and swiftly transported it vast distances across the planet to Antarctica.
Below Australia, this jet stream also contributed to blocking the eastward passage of a high pressure system. When the tropical air collided with this so-called “blocking high”, it caused the most intense atmospheric river ever observed over East Antarctica. This propelled the tropical heat and moisture southward into the heart of the Antarctic continent.
Luck was on Antarctica’s side
The event caused the vulnerable Conger Ice Shelf to finally collapse. But the impacts were otherwise not as bad as they could have been. That’s because the heatwave struck in March, the month when Antarctica transitions to its dark, extremely cold winter. If a future heatwave arrives in summer – which is more likely under climate change – the results could be catastrophic.
Despite the heatwave, most inland temperatures stayed below zero. The spike included a new all-time temperature high of -9.4°C (15.1°F) on March 18 near Antarctica’s Concordia Research Station. To understand the immensity of this, consider that the previous March maximum temperature at this location was -27.6°C (-17.68°F). At the heatwave’s peak, 3.3 million square kilometres in East Antarctica – an area about the size of India – was affected by the heatwave.
The impacts included widespread rain and surface melt along coastal areas. But inland, the tropical moisture fell as snow – lots and lots of snow. Interestingly, the weight of the snow offset ice loss in Antarctica for the year. This delivered a temporary reprieve from Antarctica’s contribution to global sea-level rise.
Learning from the results
So what are the lessons here? Let’s begin with the nice bit. The study was made possible by international collaboration across Antarctica’s scientific community, including the open sharing of datasets. This collaboration is a touchstone of the Antarctic Treaty. It serves as a testament to the significance of peaceful international cooperation and should be celebrated.
Less heartwarmingly, the extraordinary heatwave shows how compounding weather events in the tropics can affect the vast Antarctic ice sheet. The heatwave further reduced the extent of sea ice, which was already at record lows. This loss of sea ice was exacerbated this year resulting in the lowest summer and winter sea ice ever recorded. It shows how disturbances in one year can compound in later years.
The event also demonstrated how tropical heat can trigger the collapse of unstable ice shelves. Floating ice shelves don’t contribute to global sea-level rise, but they acts as dams to the ice sheets behind them, which do contribute.
This research calculated that such temperature anomalies occur in Antarctica about once a century, but concluded that under climate change, they will occur more frequently.
The findings enable the global community to improve its planning for various scenarios. For example, if a heatwave of similar magnitude hit in summer, how much ice melt would there be? If an atmospheric river hit the Doomsday glacier in the West Antarctic, what rate of sea level rise would that trigger? And how can governments across the world prepare coastal communities for sea level rise greater than currently calculated?
This research contributes another piece to the complex jigsaw puzzle of climate change. And reminds us all, that delays to action on climate change will raise the price we pay.
This article has been amended to correct an error in converting a 40°C temperature difference from Celsius to Fahrenheit.
Dana M Bergstrom, Honorary Senior Fellow, University of Wollongong
This article is republished from The Conversation under a Creative Commons license. Read the original article.
Wednesday, 23 November 2022
State of the Climate Report 2022 - climate change continues to be mapped in Australia
BOM/CSIRO (c) |
- Temperature: Australia’s climate has warmed by an average of 1.47 ± 0.24 °C since national records began in 1910.
- Sea temperature: Sea surface temperatures have increased by an average of 1.05 °C since 1900. This has led to an increase in the frequency of extreme heat events over land and sea.
- Rainfall: There has been a decline of around 15 per cent in April to October rainfall in the southwest of Australia since 1970. Across the same region, May to July rainfall has seen the largest decrease, by around 19 per cent since 1970.
- There has been a decrease in streamflow at most gauges across Australia since 1975.
- Rainfall and streamflow have increased across parts of northern Australia since the 1970s.
- Fire: There has been an increase in extreme fire weather, and a longer fire season, across large parts of the country since the 1950s.
- There has been a decrease in the number of tropical cyclones observed in the Australian region.
- Decrease in snow: Snow depth, snow cover and number of snow days have decreased in alpine regions since the late 1950s.
- Ocean acidification: Oceans around Australia are acidifying and have warmed by more than 1 °C since 1900, contributing to longer and more frequent marine heatwaves.
- Sea level rise: Sea levels are rising around Australia, including more frequent extremes that are increasing the risk of inundation and damage to coastal infrastructure and communities.
Wednesday, 11 May 2022
Great Barrier Reef in Australia - coral bleaching increases in latest report
Aerial survey (c) Great Barrier Marine Park Authority |
- A total of 719 reefs were surveyed from the air between the Torres Strait and the Capricorn Bunker Group in the Great Barrier Reef Marine Park. Of these 654 reefs (91 per cent) exhibited some fomr of bleaching and a significant core of the central reef had severe or extreme bleaching.
- Coral bleaching seen from the air is largely consistent with the spatial distribution of heat stress accumulation with a larger proportion of coral cover bleached on reefs that were exposed to the highest accumulated heat stress this last Summer (late 2021 and early 2022)
- The waters around the Great Barrier Reef exceeded historical summer maximums for the hottest summer months with three distinct heat waves increasing thermal stress throughout the Central and Northern Great Barrier Reef.
- The 2022 Aerial Survey Map [shown above] illustrates the variation in bleaching observed across the reef in the second half of March. The aerial surveys were conducted by trained observers from the Great Barrier Reef Marine Park Authority and the Australian Institute of Marine Science.
Sunday, 13 March 2022
IPCC Report February 2022: Key global indictors on impact of climate change
IPCC Report February 2022: adaptation to climate change falls well behind
IPCC 2022 |
- it is unequivocal that climate change has already disrupted human and natural systems. Past and current development trends (past emissions, development and climate change) have not advanced global climate resilient development.
- climate resilient development prospects are increasingly limited if current greenhouse gas emissions do not rapidly decline, especially if 1.5C global warming is exceeded in the near term. the Report also noted that " evidence of observed impacts, projects risks, levels and trends in vulnerability, and adaptation limits, demonstrate that worldwide climate resilient development action is more urgent than previously assessed in the 5th Assessment Report".
- the rise in weather and climate extremes has led to some irreversible impacts as natural and humans systems are pushed beyond their ability to adapt.
- approximately 3.3 to 3.6 billion people live in contexts that are highly vulnerable to climate change.
- climate change impacts and risks are becoming increasingly complex and more difficult to manage. Multiple climate hazards will occur simultaneously and multiple climatic and non climatic risks will interact resulting in compounding overall risk and risks cascading across sectors and regions.
- Note a key caveat about global warming that transiently exceeds 1.5C which is termed 'overshoot'. "Depending on the magnitude and duration of overshoot, some impacts will cause the release of additional greenhouse gases and some will be irreversible even if global warming is reduced".
Monday, 10 January 2022
Global warming and the Earth's axis
Shutterstock |
Wednesday, 3 November 2021
IPCC 6th Assessment Report - the magnitude of the crisis defined
- Human induced climate change is already affecting many weather and climate extremes in every region across the globe. Evidence of observed changes in extremes such as heatwaves, heavy precipitation, droughts, and tropical cyclones has strengthened since the 5th Assessment Report.
- Global surface temperatures will continue to increase until at least mid-century under all emission scenarios considered. Global warming of 1.5C and 2C will be exceeded during the 21st century unless deep reduction in carbon dioxide (CO2) and other greenhouse gas emissions occur in the coming decades.
- Under scenarios with increasing CO2 emissions, the ocean and land carbon sinks are projected to be less effective at slowing the accumulation of CO2 in the atmosphere.
- Continued global warming is projected to further intensify the global water cycle including its variability, global monsoon precipitation and the severity of wet and dry events.
- With further global warming, every region is projected to increasingly experience concurrent and multiple changes in climatic impact-drivers.
- Low-likelihood outcomes such as ice sheet collapse, abrupt ocean circulation changes, some compound extreme events and warming substantially larger than the assessed 'very likely' range cannot be ruled out.
- Strong rapid and sustained reduction in CH4 (methane) would also limit the warming effect resulting from declining aerosol pollution and would improve air quality.
Saturday, 19 June 2021
A rise of 3 Degrees Celsius - the impact on Australia
In March this year, the Australian Academy of Science issued a stark warning on the future of this country if global warming is not actively slowed and ultimately stopped. The Academy's report charts both proven existing impacts and the effects of modelled temperature increases. The situation could not be more starkly or clearly demonstrated by the findings of the Academy which included -
Temperature rising
- the total emission reduction current pledged by the Australian and international government through the United Nations Framework Convention on Climate Change (UNFCCC) Paris Agreement, even if implemented on time will translate as an average global surface temperatures of 3 degrees Celsius (C) or more.
- the planet is well on its way to devastating climate change with average surface temperatures being at 1.1 degrees C above the pre-industrial period. Australia has had a worse outcome with warming on average by 1.4 degrees C.
- limiting climate change to 1.5 degrees Celsius in now virtually impossible.
Ecosystems
- land-based environments have been affected by drought, fire, extreme heatwaves, invasive species and disease, large scale mortality of trees, birds and tree-dwelling mammals
- rising sea levels are amplifying storm impacts damaging coastal ecosystems such as coral reefs and mangrove forests.
Australian agriculture, forestry, fisheries and food security
- reduced water availability and heat stress have contributed to reductions in profitability for broadacre crops such as wheat and barley in the magnitude of up to 22% since 2000.
- heat stress is a significant issue for livestock systems due to impacts on animal welfare, reproduction and production. Projected temperature and humidity changes suggest an increased number of heat stress days per year.
- forestry is facing growing pressure from a warming and drying climate with increased fire risks, changes in rainfall patterns and species-specific pest impacts.
Australian cities and towns
- with close to 90% of Australians living in cities and towns, climate change experience will be manifested in various ways.
- extreme heat wave conditions, bushfires and storms already place pressure on power stations and infrastructure while simultaneously increasing demand for energy supply for air conditioning.
- global sea level rises are already occuring and pose a severe risk to properties infrastructure and ecosystems with coastal flooding becoming a more regular feature. 160,000 to 250,000 coastal properties will be at risk with a rise of 1 metre in sea levels.
- climate sensitive infectious diseases such as Ross River fever and other vector borne diseases shift their geographical distribution and intensity of transmission. This will only increase as climate change increases to above 2 degrees C.
Sunday, 9 February 2020
Understanding the impact of climate change on direct weather events
The report should probably have garnered greater interest at the time of release given it was commissioned by a large commercial insurer. The overall tenor of climate debate in Australia and political dynamic would not have been conducive to ensuring it received sufficient attention.
Of note, IAG's perspective is "... the level of knowledge has now reached the stage where it is possible to make confident assessment of the impacts of climate change at larger scales and longer time frames with objective assessment of the associated levels of confidence.." This, of course, contradicts those political naysayers who believe the evidence of climate change is still contestable.
The report provides key six assessments which are summarised briefly below and given events of the past few months, many of these assessments have been shown to be accurate -
- While the frequency of named tropical cyclones in the Australian region, the proportion of the most destructive tropical cyclones has increased at the expense of the more weaker systems. Tropical cyclone risks are therefore expected to increase rapidly in south-east Queensland, north-east NSW regional followed by coastal districts in Western Australia.
- Intense short duration rainfall is expected to increase almost everywhere in Australia , resulting in more frequent flooding in urban areas and in small river catchments.
- Areas of large hail (2.0-4.9cm in diameter) and giant hail (>5.0cm in diameter) should progressively move southwards with a large increase in the risk to the regions inland from the Hunter River, southwards through the central and southern highlands of New South Wales and central to eastern Victoria.
- The multi-day impacts of east coast lows on the south-eastern seaboard of Australia are expected to increase due to wind-driven rainfall ingress, flash and riverine flooding.
- Bushfire risk, as measured by the trends in fire danger indices is likely to increase in all locations nationally leading to more frequent and extreme events and longer fire seasons.
- Sea level rise is expected to accelerate around the Australian coastline but at differing rates. It is notable that past assessments of sea level rise are lower than those that recent observations show.
The report can be accessed at this link -
IAG - NCAR Severe weather in a changing climate report