1.5: The average global temperature increase in degrees celsuis in the Paris Agreement “to limit the temperature increase to 1.5oC”, a threshold we have already almost reached.
97%: The percentage of scientists who agree that 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: Time since the planet has experienced such high levels of carbon dioxide (CO2) in the atmosphere.
1950: Year when 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 yet.
30%: The increase in acidity of the world’s oceans.
50%: The amount of the coral reef in the Great Barrier Reef affected by coral bleaching.
8 inches (203mm): Rise in global sea levels over the last century. The rate of 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%: The increase Irish winters are expected to become wetter by mid-century.
20%: The frequency of heavy precipitation events during Irish winters.
5%: Amount of average increase in Irish annual rainfall.
192%: The expected increase of people living in Irish coastal flood-prone areas.
400 Million: The Irish 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
Climate Change Science
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, also mainly by the burning of fossil fuels. Carbon dioxide (CO2) concentrations have increased by 40 percent 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 oceans and the air goes up. 
The atmosphere is not a vast, limitless space as we might imagine it. It is a thin band and is equivalent to the skin of an apple, if comparing earth to a whole 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 green house 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 longer still.
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 percent of all species could be lost this century 
On a global basis 90 percent 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 percent, causing major problems for sea crustaceans i.e. crabs, oysters etc. to form their shells and especially problematic for coral reefs. This change in acidity is causing “coral bleaching”, which kills the coral reefs, where for example 93% of all coral in the Great Barrier Reef was affected 
Sea-level rise is also being caused by the melting of land based glaciers. The two main glacial ice-sheets are Greenland and Antarctica. On Greenland summer melt on the ice sheet 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 an as yet 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 
Climate Change 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 just about 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 a very different place if it warms by 4oC by the end of the century. See link for a map of what the world will look like 4oC warmer 
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 2 oC 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% 
Future Adverse Impacts in Ireland
Sea level rise
Ocean Acidification will have harmful effects on marine organisms
More intense storms and rainfall events
Increased likelihood & magnitude of river and coastal flooding
Water shortages in summer in the east
Adverse impacts on water quality
Changes in distribution of plant and animal species
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