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Last month, 44 climate scientists from 15 countries wrote an open letter to the Nordic Council of Ministers highlighting the risk of a potential collapse of the Atlantic Meridional Overturning Circulation (AMOC), a critical ocean current system in the Atlantic Ocean. Picture Quebec City in Canada and London in the UK.
Albedo is the total reflection of incoming solar radiation by Earth. As industrial aerosols decreased due to this new regulation, particularly over the North Atlantic Ocean, the planetary albedo slightly decreased, which means that more incoming solar radiation was absorbed by the planet rather than reflected. What is albedo?
In the real ocean that is not an observed quantity. While these simulations assimilate observational data, over most of the ocean surface these are basically sea surface temperatures, but surface heat loss depends also on air temperature, wind speed, humidity, radiation and cloud cover in complex ways, all of which are not accurately known.
Just by looking at the name, you can see that a GCM is a model that simulates the circulation of Earths different physical systems like the atmosphere and ocean. The Earths atmosphere and oceans create circulations in order to mix temperature differences between regions; GCMs, or climate models, simulate these circulations quite well.
These scenarios can also reveal how forests, oceans, and other natural systems might absorb or release carbon in the future. Research published in Earth System Science Data examined how under high-emission scenarios (SSP5-8.5), the ability of forests and oceans to absorb CO weakens. Lower-emission scenarios (SSP1-2.6)
Other new studies At few other articles on this topic have also appeared recently: Allen and Merchant (2025) give a “new interpretation of the drivers of Earth’s energy budget changes and their links to ocean warming” Terhaar et al. Indeed, we estimate that the contribution from the solar cycle has been comparably large.
That’s because the parties to the London Convention and London Protocol are meeting from October 28 to November 1 in London to discuss, among other things, governance of ocean alkalinity enhancement and ocean sinking of biomass (e.g. Some are land-based, while others use the ocean. seaweed) for carbon storage.
The fact that there is a natural greenhouse effect (that the atmosphere restricts the passage of infra-red (IR) radiation from the Earth’s surface to space) is easily deducible from; i) the mean temperature of the surface (around 15ºC) and, ii) knowing that the planet is normally close to radiative equilibrium. in IPCC TAR).
That is long enough to see that there has been a noticeable trend in the Earth’s Energy Imbalance (EEI), mostly driven by a reduction in the solar radiation reflected by the planet, while the outgoing long wave radiation does not appear to contribute much. A paper last year (Goode et al., Similarly, Loeb et al.
He made some rather strange claims, such as that the Intergovernmental Panel on Climate Change (IPCC) allegedly should have forgotten that the earth is a sphere because “ most absorption of solar radiation takes place over the tropics, while there is excess emission of longwave radiation to space over higher latitudes ”.
Projections of (a) temperature (constrained), (b) Arctic sea ice area (raw CMIP6), (c) ocean pH (constrained), and sea level (d)to 2100, and (e) to 2300 (constrained). and other things worth noting – for instance, the much better and more direct graphics that they have clearly worked on a lot. Figure SPM 8. 1981) which can be seen here.
CO 2 emissions embed themselves in the atmosphere/biosphere/upper-ocean carbon cycle and have very long-term impacts (under natural conditions, some 15% of the CO 2 perturbation will still be in the atmosphere thousands of years from now). ppm, a factor of more than 200 smaller). W/m 2 for CH 4. References. Etminan, G. Myhre, E.J.
However, not only is there an obvious energy imbalance (as seen by the growth of ocean heat content), it’s actually accelerating Loeb et al., He, however, goes seriously off the rails when he estimates the impact of clouds on the radiation budget.
W/m 2 over the ocean (which translates to 0.14 2024) Looked at the impact of Chinese aerosol emission decreases from 2010 to 2020 and saw increases in North Pacific ocean temperatures. So to help people keep track, we’ll maintain a list here to focus discussions. They find a radiative forcing 0.2±0.11 W/m 2 globally).
Hot, ocean-covered exoplanets with hydrogen-rich atmospheres could harbour life and may be more common than planets that are Earth-like in size, temperature and atmospheric composition. This subset, which the researchers dub “Hycean” (hydrogen + ocean) planets, consists of planets that have radii up to 2.6 Widening the Goldilocks zone.
Manabe’s subsequent work led to the development of the GFDL GCM, initially just including the atmosphere, but eventually with an ocean, and then the transient results shown in Manabe and Stouffer (1993). The basic issue stems from the different timescales of the ocean and atmosphere. But let’s go back to the beginning.
The only region of cooling is the northern Atlantic, where climate models have long predicted just that due to a slowing of the Atlantic Ocean overturning circulation. The heating of the global ocean has been going on at a steady rate of nine zeta Joules per year for decades , which is 15 times the worldwide primary energy consumption.
Think about what is involved – biological proxies from extinct species, plate tectonic movement, disappearance in subduction zones of vast amounts of ocean sediment, interpolating sparse data in space and time, degradation of samples over such vast amounts of time. All of which adds to the uncertainty. They get an ESS around 7.7±0.6ºC
A steep decline of Antarctic sea ice may mark a long-term transformation in the Southern Ocean, and seawater intrusions beneath the Thwaites Glacier could explain its melting outpacing projections.
Biases in the Southern Ocean are less, similarly with sea ice extent or rainfall etc. It is true that *some* models have high ECS beyond what can be reconciled with our understanding of paleoclimate change, and in those models the cloud feedback particularly in the Southern Oceans is more positive than previously. This is good news.
As deeply troubling reports continue to come in about ocean waters hitting historic hot temperatures, sectors like global shipping are trying to understand the consequences of a warmer ocean and what can be done to stop the heating. So, we’re seeing the ocean heat up, lose oxygen and get bigger.
Two decades ago, in an interview with science journalist Richard Kerr for the journal Science, I coined the term the “Atlantic Multidecadal Oscillation” (AMO) to describe an internal oscillation in the climate system resulting from interactions between North Atlantic ocean currents and wind patterns.
The physics-based models describe how energy flows through the atmosphere and ocean, as well as how the forces from different air masses push against each other. Furthermore, the volume of the oceans increases from the melting of land ice. The global sea level acts like the mercury in a thermometer because warmer water expands.
The ocean retains heat for much longer than land does. Picture how a radiator heats a home. Water is heated by a boiler, and the hot water circulates through pipes and radiators in the house. Water is heated by a boiler, and the hot water circulates through pipes and radiators in the house. Oceans in the future.
He makes his living on the Turnbridge Plantation in his hometown of Hardeeville, South Carolina, 30 minutes from the Atlantic Ocean. Atlantic sea levels are rising three to four times faster than the global ocean average. Crop damage radiates inward gradually from the edges of a field, where the salt hits first.
By Deborah Pirchner, Frontiers science writer Image: Rob Lachlan As ocean temperatures rise, corals can lose their color due to heat stress. This knowledge can help with solar radiation management in marine ecosystems, including the Great Barrier Reef. Over the past two decades, coral reefs have declined at unprecedented rates.
The plastic pollution of our oceans isn’t just affecting whales and sea turtles, it also impacts the small, microscopic animals towards the bottom of the food chain,” said Susanne Menden-Deuer, coauthor of this research and a professor at the Graduate School of Oceanography, University of Rhode Island, US.
As the material breaks down over time, it releases vast quantities of microscopic particles – which due to their small size and low density, can be transported across the globe by winds and ocean currents. Altitude matters. However, exactly how microplastics are distributed in the atmosphere is not well known.
The Sabin Center wrapped up Climate Week NYC last Friday with an event exploring the opportunities and challenges posed by ocean-based carbon dioxide removal (CDR). As evidenced by the 150-plus people in attendance, ocean CDR is attracting growing attention as a possible climate change mitigation option. ground rock) into the ocean?
In a blog post last month, I wrote about the growing interest in ocean-based carbon dioxide removal (CDR), and the complex legal issues it raises. Much of the legal complexity surrounding ocean CDR stems from the fact that the ocean is a shared resource in which all countries, both coastal and landlocked, have an interest.
A fungus living in the sea can break down the plastic polyethylene, provided it has first been exposed to UV radiation from sunlight. Researchers expect that many more plastic degrading fungi are living in deeper parts of the ocean. Read the full story from the Royal Netherlands Institute for Sea Research.
For example, Antarctica acts to cool our planet by reflecting solar radiation back to space by virtue of the brightness of its snow surface. Several floating ice shelves – the massive slabs of ice that push back grounded ice from flowing into the ocean – have catastrophically broken up in a matter of days because of such melting.
Scientific reports on climate issues, as well as reports on the state of the ocean, its ecosystems, and the relevance of the ocean for climate change, play a central role in the opinion. 52-54) and acknowledged the critical role the ocean plays in regulating the climate system (para. 157 as used in para. 52, 54, 60 and 68).
Albedo The amount of solar radiation reflected from an object or surface, often expressed as a percentage. Greenhouse Gas (GHG) Any gas that absorbs infrared radiation in the atmosphere. Natural emissions of N 2 O are mainly from bacteria breaking down nitrogen in soils and the oceans. a reduction in ocean pH).
There was little discussion, either in the written statements or at the oral hearing, of so-called “marine geoengineering” activities that seek to use the ocean to combat climate change. The second category of marine geoengineering activities, known as solar radiation management or modification (SRM), do not directly target GHGs.
The correlation had been shown in a paper by an author outside the conventional scientific community, so, for good measure, Simpson added that a non-expert could not properly appreciate how atmospheric circulation affects the absorption of radiation.
First, underwater – in the sediments on the bottom of swamps, lakes, and the ocean. For other gases, the GWP depends on two different properties of the gas: how strongly it absorbs infrared radiation; and how long it stays in the atmosphere after it is emitted. W/m 2 from elevated CO 2.
Lo first became interested in this area while studying physics and astronomy at Durham University , UK, where her final-year project looked at how to calibrate telescopes to correct for atmospheric effects on the radiation they detect. To pursue this further, Lo did a PhD in atmosphere, oceans and climate at the University of Reading , UK.
An area of high pressure above the Pacific Ocean was driven eastwards through the jet stream by a “Rossby wave” – a planetary-scale fluctuation arising from the Coriolis force. The Rossby wave eventually “broke”, dumping its energy – like an ocean wave hitting the shore – to create an area of high pressure locked over western Canada and US.
Accompanied by artists’ impressions of volcanic landscapes or storms raging above shimmering oceans, such work makes distant planets feel somehow more real. But entire oceans, continents, atmospheres and even biological signatures will still be boiled down to just a few blurry pixels. Transmission spectroscopy is limited too.
The changes to the world's oceans include warming, more frequent marine heatwaves, ocean acidification, and reduced oxygen levels. 2022: What Does the Latest IPCC Report Say? The latest IPCC report assesses global sources of greenhouse gas emissions and the progress of strategies for mitigating the impacts of climate change.
Credit: NOAA Office of Ocean Exploration (CC BY-SA 2.0). No light or other source of radiation was required. By Jessica Wimmer and Prof William Martin. A deep-sea hydrothermal vent. According to one theory, the first life on Earth arose at vents like these. Life on Earth arose roughly four billion years ago.
But it is not for her work with the ocean that Carson is best remembered. In this now universal contamination of the environment, chemicals are the sinister and little recognized partners of radiation in changing the very nature of the world – the very nature of life itself."
Student in the Department of Atmospheric Science at Colorado State University Most people remember the water cycle they learned in school: water evaporates from lakes, rivers, and the ocean, air carrying this moisture rises, cools, condenses, and forms clouds, and these clouds precipitate water back down to the surface.
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