1.5: The Paris Agreement aims “to limit the temperature increase to 1.5oC”, a threshold we have almost reached.
97%: The percentage of scientists who agree that global warming trends over the past century are very likely caused by human activity.
115,000 Years: When the world was last this warm.
4 Million Years: When the planet experienced such high levels of carbon dioxide (CO2) in the atmosphere.
1950: Atmospheric CO2 levels broke records from the previous 400,000 years, sharply rising and continuing to grow.
16: Number of record-breaking hottest years since 2000, with 2016 being the hottest year to date.
28%: Rainforests are responsible for roughly one-third (28%) of the Earth’s oxygen
70%: but most of the oxygen in the atmosphere is produced by marine plants.
30%: Increase in acidity of the world’s oceans.
50%: Coral reef in the Great Barrier Reef affected by bleaching.
8 inches (203mm): Rise in global sea levels over the last century. This rise has nearly doubled in the last two decades.
50%: Up to half of all species could be lost by the end of this century.
14%: Irish winters are expected to become wetter by mid-century.
20%: Increased frequency of heavy precipitation events during Irish winters.
5%: Average increase in Irish annual rainfall.
192%: Expected increase of people living in Irish coastal flood-prone areas.
400 Million: 4.5million Irish people emit the same amount of greenhouse gases as the poorest 400 million people on the planet.
0.1%: Climate change would cost less than 0.1% of GDP a year to address.
CO2 levels over past 400,000 years
Arctic Sea-ice Decline
Sea-Level Anomaly since 1850
Light waves travel from the sun to Earth’s atmosphere. Visible light has a short wavelength and slices through the atmosphere unimpeded. Some reflects from the surface of the earth (by clouds, ice and other reflective surfaces) and is re-radiated back into space. The rest is absorbed by the natural greenhouse gas layer and some small sooty solids that are found in our atmosphere because of burning fossil fuels like coal and wood.
This natural layer of greenhouse gases (GHG) is being thickened by human activities. Carbon dioxide (CO2) concentrations have increased by 40% since pre-industrial times, mainly from fossil fuel burning, and secondly from changes in how we use our land, agriculture and deforestation. 
As the greenhouse gas layer gets thicker more of the outgoing infrared radiation (heat) becomes trapped and so the temperature of our oceans and the air goes up. 
The atmosphere is not a vast, limitless space as we might imagine. It is a thin band and is equivalent to the skin of an apple, if comparing earth to an apple. We are putting 110 million tons of global warming pollution into that small space every hour!
The planet has not experienced such high levels of carbon dioxide (CO2) in the atmosphere for 4 million years 
The world was last this warm about 115,000 years ago when sea level was 6-9 meters (20-30ft) higher than today 
The extra heat (energy) in the atmosphere has multiple effects. The intensification of the water cycle means more water is evaporated from our oceans. Also, as the air gets warmer, it can hold more water vapour (which also has a greenhouse effect). Heavy downpours get heavier, causing more flooding 
Snowpacks melt earlier in the year, leading to more spring flooding, but less water in the heat of summer.
There are longer intervals in drought-stricken areas between downpours, making droughts even worse. More water also evaporates more quickly from the soil, making droughts deeper and last longer.
The same extra heat that evaporates more water from the ocean, causing bigger downpours. Floods also pull moisture even more quickly from the soil, causing longer and deeper droughts 
Up to 50% of all species could be lost this century 
On a global basis 90% of the extra heat goes into the oceans . This is a factor in sea level rise, as the heated oceans expand.
The extra carbon dioxide that is being absorbed by the oceans, has changed the acidity of the water by 25 – 30%, causing major problems for sea crustaceans i.e. crabs, oysters, to form their shells and is especially problematic for coral reefs. This change in acidity is causing ‘coral bleaching’, which kills the coral reefs 
Sea-level rise is also being caused by the melting of land based glaciers. The two main glacial ice-sheets are Greenland and Antarctica. The summer melt on Greenland’s ice sheet has increased by 30% 
Projections suggest an increase in global sea levels in the range of 0.26 to 0.55m for the low emissions scenario and 0.52-0.98m for the high emissions scenario. However, due to a limited understanding of some of the important effects that contribute to rates of increase, a best estimate for sea level rise cannot be provided with confidence, and estimates of up to 4-6 m have been projected by some models 
Global sea level rose about 200mm (8 inches) in the last century. The rate in the last two decades, however, is nearly double that of the last century 
Causes and Effects of Climate Change
Temperature Anomalies by Country since 1850
Greenland ice loss 2002-2016
Antarctic ice loss 2002-2016
Climate Change in the News
2016 was the hottest year on record, setting a new high for the third year in a row, with scientists firmly putting the blame on human activities that drive climate change and showed 16 of the 17 hottest years on record have been this century 
The record-smashing temperatures in 2016 led to searing heatwaves across the year: a new high of 42.7C (108.9F) was recorded in Pretoria, South Africa in January; Mae Hong Son in Thailand saw 44.6C (112.3F) on 28 April; Phalodi in India reached 51.0C (123.8F) in May, and Mitribah in Kuwait recorded 54.0C (129.2F) in July.
Warmer oceans saw coral mortality of up to 50% in parts of Australia’s Great Barrier Reef and bleaching of 75% of Japan’s biggest reef 
Sea ice extent in Arctic and Antarctic reached record lows last November. The ‘almost unprecedented’ event attributed to warm temperatures and winds, with some areas more than 20C (36F) warmer than usual 
Soaring Arctic temperatures ‘strongly linked’ to recent extreme weather events, say scientists at cutting edge of climate change research and ‘already affecting weather patterns where you live right now’ 
The world was last this warm about 115,000 years ago and the planet has not experienced such high levels of carbon dioxide (CO2) in the atmosphere for 4 million years 
Avoiding dangerous levels of climate change is still possible, but will require unprecedented effort and coordination from governments, businesses, citizens and scientists in the next three years, a group of prominent experts has warned 
The world will look like a very different place if it warms by 4oC by the end of the century. Click here for a map of what the world will look like 4oC warmer 
“Chasing Ice” Trailer
NASA Climate Predictions to 2100
Climate Change in Ireland
Winters are expected to become wetter with increases of up to 14% in precipitation under the high emission scenarios by mid-century; summers will become drier with up to 20% reduction in precipitation under the high emission scenarios 
The frequency of heavy precipitation events during winter shows notable increases of up to 20% 
Declining Arctic sea ice may increase the likelihood of cold continental air outbreaks over Ireland during winter 
Sea temperatures may rise by 2oC by the end of the century, causing intense, aggressive storms 
Levels of ocean acidity in sub-surface and deep offshore waters around Ireland have increased significantly over the period from 1991 to 2010. Increasing atmospheric CO2 is expected to result in increased oceanic acidity 
Changes would result in more drought, flooding, heavy rainfall and extreme temperatures that will, in turn, lead to changes in the range and prevalence of pests and diseases, and increased stress for animals 
The mean proportion of people living in coastal flood-prone areas is expected to increase, with one of the most notable increases happening in Ireland of 192% 
Effects on fisheries sensitive to changes in temperature 
Vicente R. Barros et al., Climate Change 2014: Impacts, Adaptation, and Vulnerability. Part B: Regional Aspects. Contribution of Working Group II to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge University Press, Chapter 3 – Observations: Ocean (March 31, 2014): 257. http://www.ipcc.ch/pdf/assessment-report/ar5/wg2/WGIIAR5-PartB_FINAL.pdf
IPCC, 2013. Summary for Policymakers. In: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press. Cambridge, UK.
Gleeson, E., McGrath R. and Treanor M. (2013). Ireland’s climate: the road ahead. Dublin: Met Éireann
McGrath, T., McGovern, E., Nolan, G. &N. Dwyer, 2012. Ocean Acidification and Carbon Dioxide Concentrations. The Status of Ireland’s Climate 2012. N. Dwyer. Wexford. Environmental Protection Agency. 65-67