26 juin 2007

les reserves de gaz naturelles

Au cours des vingt dernières années, les réserves de gaz naturel en chiffres absolus ont énormément augmenté. Le Moyen-Orient, l'Europe et l'Eurasie disposent de la plus grande partie des réserves mondiales de gaz naturel. Toutefois, tout comme pour le pétrole, à la décroissance du nombre des gisements de gaz naturel exploités s'oppose une croissante demande d'énergie.

Les faits

Les réserves de gaz naturel confirmées ont augmenté de 96,4 billions de m³ en 1984 à 179, 5 billions de m³ à l'échelle mondiale en 2004. En 2004 le Moyen-Orient détenait 40,6% des réserves mondiales de gaz naturel et l'Europe et l'Eurasie 35,7%. Ces régions détiennent ainsi à elles seules la plus grande partie des réserves mondiales, tandis que la région asiatique du Pacifique ensemble avec l'Afrique n'en détiennent que 8% et que l'Amérique du Nord, l'Amérique centrale et l'Amérique du Sud ne dispose chacune d'elle que de 4% des réserves.

Comme pour le pétrole, l'augmentation des réserves de gaz naturel en termes absolus dans le passé ne change rien au fait que la mise en exploitation de nouveaux gisements de gaz naturel baisse, tandis que sa consommation augmente. Le jour où l'approvisionnement en gaz naturel dépassera la croissance des réserves semble assez proche pour le gaz aussi. À long terme, le gaz ne compensera pas l'épuisement des réserves de pétrole. D'après les prévisions de la compagnie pétrolière et gazière BP, l'écart qui existe entre le développement réserves de gaz naturel et la consommation grandissante de gaz n'est plus très large. Entre 2004 et 2005 les réserves de gaz ont à peine augmenté de 0,83 billions de m³, tandis que sa consommation a fait un bond de 2,75 billions m³.

Toujours d'après BP, qui calcule les .réserves de gaz naturel partant de la production annuelle, il ne nous reste plus que 65,1 ans jusqu'à l'épuisement total des réserves si les conditions actuelles se maintiennent. En 1981 l'approvisionnement en gaz jusqu'à l'épuisement total des réserves avait été estimé à soixante ans. La mise en exploitation de nouveaux gisements a repoussé cette estimation, en 2001, jusqu'à 70 ans. Si chaque région ne pouvait compter que sur ses propres réserves, l'ensemble de l'Amérique du Nord devrait se passer de gaz d'ici dix ans déjà. L'Europe et l'Eurasie serait tout juste au-dessous de la moyenne mondiale. Seul le Moyen-Orient aurait assez de réserves pour maintenir sa consommation actuelle pendant encore 250 ans.

Comme pour le pétrole, des voix critiques attirent l'attention pour le fait que les chiffres donnés par les compagnies pétrolières et gazières, partant du principe que les réserves de gaz naturel sont elles aussi limitées, seraient trop optimistes. La première raison pour une surestimation est que la hausse des réserves s'inscrit positivement dans le bilan de la compagnie et donc aussi pour la cotation en bourse de ses sociétés. La tentation est donc grande, dans le doute, de partir de la supposition que les réserves sont importantes. D'autre part, les pays producteurs de gaz naturel auraient, eux aussi, l'intérêt d'afficher des réserves importantes afin de ralentir la poussée des énergies alternatives. Aussi bien pour le pétrole que pour le gaz il manque des données objectives, étant donné que les chiffres avancés proviennent d'un milieu où règnent intérêts économiques et politiques.

Sources d'information

British Petroleum (BP): Statistical Review of World Energy 2005

Notions, notes méthodologiques et conseils de lecture

Les réserves de gaz naturel et les ressources de gaz naturel sont deux choses différentes. Le terme «ressources» de gaz naturel désigne les gisements existants, que ceux-ci soient exploitables ou pas même encore découverts. Les «réserves» de gaz naturel sont uniquement les ressources de gaz naturel qui sont exploitables et rentables aux prix courants.

En chiffres absolus et en pourcentage, 1984, 1994, 2004.

Réserves de gaz naturel en billions de m³
1984 1994 2004
Monde* 96,39 142,89 179,53
Moyen-Orient 27,38 45,58 72,83
Europe et Eurasie 42,03 63,87 64,02
Région asiatique du Pacifique 7,04 10,0 14,21
Afrique 6,17 9,15 14,06
Amérique du Nord 10,51 8,43 7,32
Amérique centrale et du Sud 3,28 5,86 7,1

Pourcentage sur les réserves mondiales
1984 1994 2004
Monde* 100 100 100
Moyen-Orient 28,04 31,9 40,6
Europe et Eurasie 43,6 44,7 35,7
Région asiatique du Pacifique 7,3 7,0 7,9
Afrique 6,4 6,4 7,8
Amérique du Nord 10,9 5,9 4,1
Amérique centrale et du Sud 3,4 4,1 4,0


*D'éventuels décalages sont possibles dû à l'arrondissement des chiffres.

Eurotopics

6 juin 2007

Les derniers chiffres du climat de Janvier à Avril 2007 : +0,5°C au dessus de la moyenne

News release

5 June 2007

Climate figures revealed as G8 leaders prepare to meet

As G8 leaders meet in Germany this week to discuss global issues such as climate change, the Met Office has revealed figures showing that the mean global temperature for the period January to April was almost 0.5 °C above the long-term average.

The Met Office global temperature forecast predicted that 2007 had a 60% probability of being the warmest on record, with a mean temperature 0.54 °C above the long-term (1961-1990) average of 14 °C.

David Parker, a climate variability scientist at the Met Office Hadley Centre said: "These latest Met Office figures show that the first four months of 2007 are on track with our global forecast for a warmer-than-average year, but the cool La Nina event developing in the equatorial Pacific could prevent 2007 from being the warmest ever year".

Met Office figures also reveal that this spring has been the warmest since UK-wide records began in 1914. The UK mean temperature for Spring 2007 was 9.0 °C, beating the previous record of 8.8 °C set in 1945. The three spring months of March, April and May all exceeded their long-term average temperatures.

The warm UK spring follows one of the warmest recorded winters, and a run of record breaking years – the last five years are the warmest on record – and this warming trend is consistent with our predictions from the Met Office Hadley Centre.

The Met Office works with government and other organisations by offering advice on the possible consequences and risks of climate change.

Provisional spring figures for the UK nations

Mean Spring 2007 temperature Previous or current record Year of previous or current record
UK 9.0 °C 8.8 °C 1945
England 9.9 °C 9.6 °C 1945
Northern Ireland 9.0 °C 9.1 °C 1945
Scotland 7.6 °C 7.6 °C 2003
Wales 9.1 °C 9.0 °C 1945

Spring 2007 summary

More about G8 Summit 2007

Notes:

  • The Central England Temperature (CET) is the world’s oldest temperature series and dates back to 1659. Spring 2007 has been the second warmest on record with a mean temperature of 10.1 °C. The warmest spring was in 1893 with a mean temperature of 10.2 °C.
For further information:
Met Office Press Office +44 (0)1392 886655
E-mail: pressoffice@metoffice.gov.uk

Met Office Customer Centre 0870 900 0100
If you're outside the UK +44 (0)1392 885680

5 juin 2007

flux migratoires

Un article alertant sur les flux migratoires à telecharger :

le rapport "Marée humaine, la véritable crise migratoire" en anglais (pdf, 2 Mo)


en voici un extrait ...

The number of natural disasters has more than doubled over

the last decade, from 193 in 1996 to 422 in 2005, according to

the IFRC.17

The increase is due to a sharp rise in the number of

weather-related disasters – from 175 in 1996 to 391 in 2005 – an

upward trend that will continue because of climate change.

Poor people are especially vulnerable to displacement by

natural disasters, because their poverty forces them to live in

less favourable places which, for instance, are more prone

to flooding or landslides. Their less-robustly built homes are

similarly more vulnerable to destruction by extreme weather

and earthquakes.18

People who are already displaced from their homes by

conflict or large-scale development projects are also particularly

badly affected by natural disasters. This was evident among the

tens of thousands of people already displaced by the conflicts in

Sri Lanka and Indonesia when the tsunami hit on Boxing Day 2004.

The UN’s expert on the human rights of IDPs, Walter Kälin,

visited the region for the UN Secretary General on the Human

Rights of Internally Displaced Persons. ‘Many observers noted

that in areas already affected by conflict and hosting IDPs, there

had in some cases been unequal treatment in the assistance

provided by governments and international actors, in particular

certain NGOs,’ he reported.

For example, UK

company Asia Energy admits that operating its planned opencast

coal mine in Phulbari, Bangladesh, would require 40,000

people to leave their homes.

And, ironically in the light of Bangladesh’s extreme

vulnerability to rising sea levels caused by climate change, which

could displace 35 million people,32 the mine will displace people

from valuable high ground because it is some 30 metres above

sea level, according to Asia Energy. Burning the coal that comes

out of the mine will produce more of the very greenhouse gases

that are causing climate change.

Opposition to the mine provoked protests in which at least

three people were killed and 200 injured last year, according to

the BBC.33 The government of Bangladesh then postponed a

decision on the future of the mine until after elections that were

due to take place in January this year. However, political violence

caused the elections to be postponed; it is now hoped that they

will take place later this year.

The latest Intergovernmental Panel on Climate Change

(IPCC) report highlights the huge numbers of people who are

predicted to suffer a severe impact from climate change. Most

of the references here are taken from unpublished drafts of the

report because, as this report goes to press, the full text is not

available.1

By 2080, it is likely that 1.1 to 3.2 billion people will be

experiencing water scarcity; 200 to 600 million, hunger; 2 to 7

million more per year, coastal flooding,’ says the IPCC.2

‘Stresses such as increased drought, water shortages and

riverine and coastal flooding will affect many local and regional

populations. This will lead in some cases to relocation within

or between countries, exacerbating conflicts and imposing

migration pressures.’3

As this suggests, climate change will displace people from

their homes, both directly and by intensifying conflicts that

cause people to flee. Military planners have been worrying

about such scenarios for years, and have reached alarming

conclusions.

Floods and water shortages

Studies of the effects of climate change on human beings

suggest a future in which millions more people will suffer

extreme events such as tidal waves, droughts, floods and

hurricanes, and the poorest will be hardest hit. Indeed, there

is strong evidence that it is already biting, as the latest IPCC

report points out.

The number of disasters caused by weather-related

phenomena such as hurricanes, floods and droughts has more

than doubled over the past decade, from 175 in 1996 to 391 in

2005.6 The proportion of the world that is affected by drought

has risen substantially since 1980, according to the climate

change experts at the UK Met Office’s Hadley Centre for

Climate Prediction and Research.7

There is high-level recognition that such changes will,

in some cases, force people to leave their homes. The

Stern Review warned: ‘As temperatures rise and conditions

deteriorate significantly, climate change will test the resilience

of many societies around the world.

Large numbers of people

will be compelled to leave their homes when resources drop

below a critical threshold. Bangladesh, for example, faces the

permanent loss of large areas of coastal land, affecting 35

million people (about one-quarter of its population), while onequarter

of China’s population (300 million people) could suffer

from the wholesale reduction in glacial meltwater.’8

The latest IPCC impact report warns that it is the regions

already struggling with other problems which force people

from their homes that are most vulnerable to the effects of

climate change: ‘Vulnerable regions face multiple stresses

that affect their exposure and sensitivity [to climate change] as

well as their capacity to adapt. These stresses arise from, for

example, current climate hazards, poverty and unequal access

to resources, food insecurity, trends in economic globalisation,

conflict and incidence of diseases such as HIV/AIDS.’9

The IPCC also highlights the vast numbers of people

around the world who are at risk from flooding by the sea.

‘In the absence of an improvement to protection, coastal

flooding could grow tenfold or more by the 2080s to more than

100 million people a year, just due to sea-level rise alone.’10

In Africa, it suggests that without mitigation of climate change

and adaptation to its effects, between 350 million and 600

million people would suffer increased water scarcity if global

temperature were to rise by 2°C over pre-industrial levels.11

This, in turn, would affect their ability to grow food. ‘In some

countries, yield from rain-fed agriculture could

In Asia and Latin America, water shortages will be a major

problem, with a 2°C rise in temperature affecting between 200

million and 1 billion people in Asia, and 80 to 180 million people

in Latin America.13

A report released by the Hadley Centre in 2006 warned

that very large increases in both the spread and the severity

of droughts will leave almost a third of the planet with extreme

water shortages by the end of this century.14

As well as the increased frequency of extreme events that

climate change will bring, there will be other impacts that also

push people from their homes. Gradual changes in regional

and local climates – for example slowly decreasing rainfall – are

likely to undermine people’s ability to make a living – especially

for the 1 billion people in the world who currently rely on

smallholder agriculture for their survival and income.

Steadily and silently, people will be forced to leave their

land and seek alternative means of survival elsewhere. The

likelihood is that people displaced in this way will migrate to

the nearest town or city, accelerating the pace of rural to urban

migration or perhaps, in time, further afield.

This will put increasing strain on already overburdened

urban infrastructure, but it may also fail to deliver people from

the impact of climate change – many of the places to which

they will naturally gravitate, such as large coastal cities, will also

increasingly be at risk.

This slow-onset crisis can be prevented. But to achieve this

it is essential that drastic action is taken to cut CO2 emissions

globally in order to keep average temperature increases to

below 2°C. Furthermore, additional funds must be released to

help people adapt the way they live to cope with an increasingly

harsh climate.

Regions where climate change holds the greatest risk of

creating population displacement include countries that

are already wracked by conflict and are hosts to groups

that pose security concerns internally and internationally.’

Professor Robert McLeman of the University of Ottawa, Canada

Oumou and Ibrahim Karembé with four of their seven young

grandchildren outside their stone hut in the village of Solo-Joy,

northern Mali. All eight of their children have been forced to leave

the village because there is not enough rain for their crops

Oumou Karembé has four sons and four daughters. More

than enough to look after her in her old age, she thought. But

that was in the days when enough rain fell – most of the time

– to sustain the farmers living in Africa’s Sahel region. After the

massive droughts in the early 1980s, Oumou’s village never fully

recovered. Indeed, since then, the rain has become less and

less predictable. Two years ago, the last of Oumou’s sons was

forced to leave the remote village in northern Mali because he

could no longer feed his family with what he was able to grow.

Now aged 76, she sits on a straw mat in her stone hut,

sheltering from the 35°C heat with her 79-year-old husband. At

a time when she could expect a rest from the back-breaking

work she has endured her whole life, Oumou instead has

seven young grandchildren to look after, aged between 18

months and 15 years.

One son has agreed to come back and help during the

growing season, and his parents say they will do everything

possible to convince him to stay for good – even crying openly

in front of him if that’s what it takes.

‘One by one my children asked permission to leave,’ said

Oumou’s husband, Ibrahim. ‘Every time they didn’t come

back, it was a shock. But with the changing climate it would be

difficult for them all to stay here.’

The Sahel region is a swathe of land stretching across Africa

from Senegal on the Atlantic coast to Somalia on the Indian

Ocean. This region, which cuts across the north of Mali, is what

is known as a semi-arid area, between highly fertile land and

the desert, where agriculture is very vulnerable to changes in

rainfall patterns. Mounting evidence suggests that the effects

of global warming are already being felt throughout the Sahel

– changing the delicate balance between humans and their

environment that has endured for thousands of years. A study

published by the UK Met Office’s Hadley Centre for Climate

Prediction and Research last year found that extreme drought

is liable to affect a third of the planet by 2100. Places which are

already suffering periodic droughts and unpredictable rains will

get progressively drier and the Sahel will eventually become

uninhabitable.1

Many Malian farmers are already noticing changes

consistent with these predictions, and the country’s rainfall

data further supports this view. Over the past 30 years, the

rainfall on which the farmers depend has lessened dramatically

and has become much more erratic (see graph below). Once,

farmers could predict the rains and plant accordingly. During the

past five years, farmers report rain disappearing in the middle

of the growing season, which drastically reduces, if not totally

destroys, their crops.

This change in rainfall patterns is creating a new wave of

migrants who are being driven from their homes in search of

water, leaving the very old and the very young in the villages to

cope as best they can. Already the third poorest country in the

world, the fragile Malian economy is facing yet another shock.

While we have made the technological and logistical advances

necessary to send teams rapidly anywhere in the world, there has

been no corresponding moral and ethical revolution by the global

community to make it possible to assist and protect everyone

everywhere in accordance with humanitarian principles and our

agreed responsibility to protect.’

Jan Egeland, former United Nations Under-Secretary-General for Humanitarian Affairs and Emergency Relief Coordinator

Climate change

Scientific forecasts about the effects of climate change are

frightening. They suggest a world in which people in already poor

countries will have an even harder struggle to survive. Although

there are no up-to-date statistics to show how many people are

being displaced by climate change, it is clear that the numbers

are potentially in the hundreds of millions. This, in turn, is likely to

fuel conflicts that will push still more people to flee.

It is poor people who will suffer most as a result of climate

change, but rich people who are most to blame for it. In sub-

Saharan Africa, people emit less than one tonne of CO2 per

year while in the US it is 24 tonnes.

The latest scientific studies suggest that the climate is

changing more quickly than was previously predicted. In

addition, because of international prevarication over reducing

CO2 emissions, the scale and speed of action needed now is

greater than previously imagined. A massive, international effort

is needed to reduce CO2 emissions and keep global average

temperature increases below 2°C. Even then, climate change

will cause serious disruption, especially in poor communities.

A new international, science-based and equitable agreement

is needed along the lines of a ‘global carbon budget’. This

must be consistent with the 2°C-limit and recognise the right

of developing and less-developed countries to increase the

size of their economies and reduce poverty in a way that

does not lead to further growth in global CO2 emissions.

The agreement should have at its heart development-friendly

mechanisms with which rich countries will fund adaptation

and clean-development activities in poor countries.

As part of the agreement, rich countries that have emitted

most pollution must establish a US$100 (£50) billion a year

global fund to help poor, vulnerable counties to adapt to sealevel

rises, increasing drought and more extreme weather.

Funding could be based on CO2 taxation or trading, or both.

This money should not be taken from existing aid budgets

– it is partial compensation for the damage done by climate

change. It should be paid in proportion to countries’ CO2

emissions since 1990 (when negotiations on the UN

Framework Convention on Climate Change began), and

national wealth.

In addition, it is in all countries’ interests to share and develop

low-carbon technology and pass on know-how. The costs

of this should be borne by rich countries, and intellectual

property rights should not stand in the way of stabilising the

amount of CO2 in the atmosphere. At the Conference of the

Parties to the Framework Convention on Climate Change, the

importance of discussions on technology transfer should be

elevated, with rich countries taking seriously their obligations

in Article 5 to take ‘all practicable steps’ to ‘promote, facilitate

and finance’ technology transfer.

In the short term, financial support for adaptation should be

increased via more rapid debt cancellation and increases in

overseas development assistance. In addition, rich countries

must live up to the pledges they have made to help the poor

cope with climate change.

The UK should pay all the money it has pledged to the climate

change funds without delay. Pledging £10 million but staging

payments over three years harms the adaptation efforts of

the poorest countries in the world.

The UK should lead the way towards a science-based,

equitable international agreement and towards mechanisms

to fund clean development and adaptation in countries that

have limited resources to deal with them.


31 mai 2007

4ème rapport du GIEC

4ème rapport du GIEC : les conclusions du Groupe III

CO2.jpg

Les conclusions du Groupe III du 4° rapport du GIEC ont été présentées à Bangkok le 4 mai 2007. Vous pouvez les télécharger sous la forme d’un résumé en anglais.

Le point important de ce rapport c’est la teneur en CO2 de l’atmosphère, qui augmente plus vite que prévu.

Dans les années 90, le taux de croissance du CO2 était en moyenne de 1% par an. Entre 2000 et 2005, il est de 3%.

L’augmentation du CO2 était prévue par les modèles, elle est dûe à l’accroissement de la population mondiale et au développement industriel accéléré de pays comme l’Inde ou la Chine. Par contre, ce qu’on avait pas prévu, c’est que les plantes et les océans piègent moins de dioxyde de carbone que prévu, ce qui fait que le réchauffement est en train de s’emballer.

C’est d’ailleurs ce que vient de confirmer une étude du British Antarctic Survey. Les "puits de carbone" piègent la moitié du CO2 produit par l’activité humaine. L’Océan Antarctique y participe pour 15%. Cette étude montre que la capacité d’absorption de CO2 de l’Océan Antarctique arrive à saturation, et que l’acidité de l’Océan Antarctique risque d’atteindre la cote d’alerte bien avant 2050, comme on le pensait jusqu’à présent.

Le Professeur Chris Rapley, Directeur du British Antarctic Survey a déclaré : "Depuis le début de la révolution industrielle, les océans du globe on absorbé environ un quart des 500 gigatonnes de carbone émis dans l’atmosphère pas l’activité humaine. La possibilité que le réchauffement climatique puisse réduire la capacité d’absorption du CO2 dans l’Océan Antarctique (le plus puissant "puits de carbone") est à prendre très au sérieux."

Pour en savoir plus :
1. Climate Change 2007 : Mitigation of Climate Change (IPCC WGIII - fichier .pdf)
2. 4° rapport du GIEC - les conclusions du Groupe II (Gaïa)
3. Les émissions de CO2 s’envolent depuis 2000 (Le Figaro)
4. Polar ocean ’soaking up less CO2’ (BBC news)
5. Climate change affects Southern Ocean carbon sink (British Antarctic Survey)
6. L’Océan Antarctique absorbe moins de CO2 que prévu (notre-planete.info)

Crédit illustration : IPCC

savez vous calculer les émissions de CO2 du Porshe Cayenne ?

« L'objectif affirmé de Porsche est de réduire au minimum les effets préjudiciables à l'environnement, et de soutenir également les efforts internationaux visant à résoudre les problèmes écologiques globaux. »
Site internet de Porsche.


Nouveau Porsche 4 x 4 Cayenne : poids 2 tonnes et demi , 450 Chevaux, 266 Km/h.

Je n'ai rien contre les 4x4 (sauf pour aller chercher du pain à 5' de chez soi) parce qu'une 806 ça crache presque autant .., mais bon... là de là à dire que l'objectif de Porshe est de réduire les effets préjudiciales à l'environnement ! ils poussent le bouchon un petit peu loin je trouve

29 mai 2007

un site à connaire : terra-economica (remettez l'homme au coeur de l'économie)

http://www.terra-economica.info/-Enquete-.html

articles interessants, notamment sur les quartiers éco-conçus en chine ou en autriche

semaine de la mobilité

Pour participer à la Semaine européenne de la mobilité, il vous suffit :
1. d'organiser, pendant la Semaine, une ou plusieurs actions visant à promouvoir les moyens de transports respectueux de l'environnement (transports en commun, vélo, marche, covoiturage, autopartage...) en faveur de changements de comportements en matière de déplacements.
2. d'inscrire votre projet, en remplissant le formulaire en ligne sur le site www.bougezautrement.gouv.fr.

Vous n'avez jamais participé et ne savez pas quel type d'action organiser ? Consultez les exemples d'actions, sur le site de l'opération, dans la rubrique qui vous concerne.



Pour plus d'informations, consultez la note d'organisation de l'opération (http://www.ecologie.gouv.fr/bougezautrement/IMG/pdf/Note_d_organisation_SEM_2007.pdf) ou contactez vos interlocutrices au ministère de l'Ecologie, du Développement et de l'Aménagement durables :
> Emilie Pitard, au 01 42 19 20 29 - emilie.pitard@ecologie.gouv.fr
> Catherine Veyer, au 01 42 19 19 45 - catherine.veyer@ecologie.gouv.fr

24 mai 2007

les risques potentiels du réchauffement climatique

Suite à mon post "gaz à effets de serre pour les nuls", voici maintenant quelques risques identifiés plus ou moins probables du réchauffement climatique à venir (au minimum 2°c en 100 ans pour rappel) tels que je les ai compris

Avant de me lancer là dedans, une précaution : je ne suis ni catastrophiste, et je ne suis nullement rémunéré par aucune association écolo...mais j'essaye en écrivant ces quelques lignes d'y voir plus clair moi-même et c'est loin d'être simple !

Risques n°1 : impacts sur les écosystèmes (affaiblissement, disparition, déplacement), naturels et domestiques (agriculture). Celui-là je ne le maitrise carrément pas, à approfondir ..

Risques n°2 : Augmentation du niveau des océans
d'après le GIEC, au minimum (pour l'hypothèse de réchauffement la plus basse de 2°), l'élévation du niveau des océans serait au minimum de 10 cm en 2100, au maximum 80 cm, ce qui provoquera :
- des inondations de surfaces terrestres peu élevées (toutes les zones avec des deltas). La capacité de réaction de pays évolués comme la Hollande permettra de trouver temporairement des solutions, mais dans les pays les moins armés il sera beaucoup plus difficile de réagir..
- la salinisation possible des nappes phréatiques proches des côtes
- des dégâts plus importants lors de tempêtes
En 2050, nous atteignons déjà une élévation de 5 cm au minimum

Risques n°3 : doublement de la proportion des cyclones puissants (catégories 4/5) par rapport aux cyclones plus faible d'ici 30 ans
Le nombre de cyclones ne devrait pas augmenter mais leur puissance oui . La corrélation est très forte entre la température moyenne de l'atlantique tropical et l'energie libérée par les cyclones

Risque n°4 : l'emballement des émissions de Co2 générées par les "puits de Co2" qui deviennent des "sources à CO2"
- du fait du réchauffement, les sols des forêts par augmentation de l'activité microbienne, au delà d'un certain seuil, se transformeront en source de CO2 au lieu d'être des "sequestrateurs de CO2" (pour comprendre un peu plus, allez voir mon post sur "les gaz à effets de serre" pour les nuls)
- de même pour la végétation (par stress hydrique)
- ce qui génère un phénomène d'amplification des émissions de CO2 au delà d'un seuil d'émission
- en 2003 ce phénomène est déjà apparu en Europe : l'Europe a déstocké 4 années de séquestration du CO2 en 2003. ce phénomène n'est donc pas inédit, il s'est déjà produit !
(source : Ciais et al., Nature, septembre 2005)
- les pergélisols (partie du sol située sous la surface qui ne dégèle pas pendant au moins 2 années consécutives, soit 25% des terres émergées !) contiennent du méthane sous formes d'hydrates solides qu'un début de réchauffement pourrait émettre de manière massive dans l'atmosphère