this post was submitted on 11 Nov 2023
40 points (100.0% liked)

Climate - truthful information about climate, related activism and politics.

5212 readers
809 users here now

Discussion of climate, how it is changing, activism around that, the politics, and the energy systems change we need in order to stabilize things.

As a starting point, the burning of fossil fuels, and to a lesser extent deforestation and release of methane are responsible for the warming in recent decades: Graph of temperature as observed with significant warming, and simulated without added greenhouse gases and other anthropogentic changes, which shows no significant warming

How much each change to the atmosphere has warmed the world: IPCC AR6 Figure 2 - Thee bar charts: first chart: how much each gas has warmed the world.  About 1C of total warming.  Second chart:  about 1.5C of total warming from well-mixed greenhouse gases, offset by 0.4C of cooling from aerosols and negligible influence from changes to solar output, volcanoes, and internal variability.  Third chart: about 1.25C of warming from CO2, 0.5C from methane, and a bunch more in small quantities from other gases.  About 0.5C of cooling with large error bars from SO2.

Recommended actions to cut greenhouse gas emissions in the near future:

Anti-science, inactivism, and unsupported conspiracy theories are not ok here.

founded 1 year ago
MODERATORS
 

Because of its growing impact on society, global warming has taken centre stage in the public debate. While most of us have not read the reports by the Intergovernmental Panel on Climate Change (IPCC), heat waves, intensifying storms and the multiplication of extreme events remind us of the scale of climate disruption and the urgency of action.

Despite being documented by the Intergovernmental Sciences Policy Platform on Biodiversity and Ecosystem Services (IPBES), the equivalent of the IPCC for biodiversity, we know little about how biodiversity erosion might affect us and the rest of the planet. Its links and interactions with climate change are underestimated, and any policy to address either in isolation will miss the mark. It’s impossible to take effective action against global warming without addressing our impact on the rest of the living world, and vice versa.

(...)

IPCC scientists have been explaining since their first assessment report (1990) that climate change is a stock problem. To halt global warming, it is not enough to slash greenhouse gas emissions. We need to stabilise their stock in the atmosphere. To achieve reach net zero we must reduce emissions – the inflow into the stock – to the level of the outflow, which is made up of CO2 absorption by carbon sinks (forests and oceans) and the elimination of non-CO2 greenhouse gases at the end of their life cycle. (...)

On the other hand, a quarter of greenhouse gas emissions come from “living carbon”, mainly as a result of specific agricultural emissions (unrelated to fossil fuel use) and tropical deforestation and other land use changes that erode carbon sinks. There is no way to achieve carbon neutrality without a profound transformation in the use of living resources, to ensure the reflux of agricultural emissions and better protection of carbon sinks. This is the challenge of what we might call the agroclimatic transition.

One of the major difficulties of the ecological transition is to carry out these two transformations simultaneously, as they involve distinct economic mechanisms. For fossil carbon, we need to introduce scarcity by reducing the use of coal, oil and natural gas to the absolute minimum. For living carbon, we need to reinvest in the diversity of ecosystems to reduce agricultural emissions and protect carbon sinks as part of a bioeconomy.

From adding to subtracting

Since the start of the Industrial Revolution, energy transitions have followed one another. They have all involved adding new energy sources to a system initially based on the use of biomass. The result has been a massive increase in the amount of energy used worldwide.

The climate is forcing us to break with this logic. Lowering emissions is not a matter of adding decarbonised sources to the energy system. It’s about removing fossil fuels. We need to switch from a logic of addition to one of subtraction. (...)

Multiple instruments will have to be called upon to bring about such a transformation. Pricing carbon from fossil fuel use is a key way to reflect the increasing scarcity of the atmospheric capacity to store carbon. Whether obtained through taxation or emission trading schemes, such taxation raises the cost of using fossil fuels, without returning the resulting rents to producers, as happens, for example, when oil prices soar on energy markets. On the demand side, it is a powerful stimulus to energy efficiency and sufficiency; on the supply side, it encourages a shift away from carbon assets.

The main difficulty with fossil carbon taxation lies in controlling its distributive impact. As the “gilets jaunes” protests in France showed, fossil carbon taxation without redistribution to the most vulnerable poses more problems than it solves. Only a redistributive carbon tax will be socially acceptable. Similarly, if carbon pricing is to be extended on an international scale, the proceeds must be returned on a massive scale to the countries of the South.

(...)Another pernicious form of subsidy to fossil fuels is the free allocation of CO2 allowances in the European trading scheme, which hampers the emergence of a green industry, a lever for the competitiveness of tomorrow’s Europe.

Investing in the diversity of living beings

Let’s imagine for a moment that the world has eradicated all use of fossil fuels in 2050. Would we automatically be in a situation of climate neutrality? Everything depends on what has been achieved on the second front of the transition, that of living carbon, the source of a quarter of the world’s greenhouse gas emissions. (...) Agro-climatic transformation means finding ways to reinvest in biological diversity, in other words, in the abundance of living things. But the price of CO2 does not reflect the value of this diversity. We therefore need to use other instruments, which are more complex to implement.

On land, forests are the main carbon sink. Their capacity to soak up atmospheric CO2 is weakened by a combination of climatic and anthropogenic factors. In France, for example, the CO2 storage capacity of forests has been divided by three since 2005, mainly due to climatic factors. There is therefore an urgent need to adapt forest management methods in anticipation of the severity of tomorrow’s climates.(...)

The key issues of agriculture and food

The impact of farming systems on the net balance of greenhouse gas emissions is not limited to deforestation. Depending on the techniques used, farming systems may themselves release carbon into the atmosphere (deep ploughing, draining of wet soils, etc.) or, on the contrary, store it in living soils (conservation agriculture, agroforestry, etc.). The former erode biodiversity by specialising farmers according to industrial-type logics. The latter use living diversity to intensify production and regenerate the natural environment.

(...) In economic terms, their promotion requires investment in innovation, research and development, the establishment of dedicated farm advisory networks and, above all, incentivisation to reward farmers for the ecosystem services they provide to society. This is not something that happens spontaneously on the market. It requires public intervention and dedicated funding.

As in the case of energy, the agroclimatic transition implies, on the demand side, that we consume smarter and less. The foods we eat have contrasting climate footprints. There can be no successful agroclimatic transition without finding ways to dramatically reduce emissions associated with the most polluting ingredients, including industrially processed foods and animal products(...)

Remembering the ocean

Last but not least, the agroclimatic transition will have to take into account the management of the oceans and marine biodiversity, which are currently the blind spots of climate policies. Global warming and certain human practices (overfishing, pollutant runoff, etc.) are altering marine biodiversity, a crucial component in the storage of CO2 by the oceans. Protecting the ocean sink is vital to stabilise tomorrow’s climate: it is estimated that the continental biosphere contains four times more carbon than the atmosphere. For the oceans, it’s 47 times.

Christian de Perthuis Professeur d’économie, fondateur de la chaire « Économie du climat », Université Paris Dauphine – PSL
Édouard Civel Chercheur au Square Research Center et à la Chaire Economie du Climat, Université Paris Dauphine – PSL

no comments (yet)
sorted by: hot top controversial new old
there doesn't seem to be anything here