Shell building and calciferous marine organisms, coral reefs and some algae production may suffer with increased acidity. The acidification of the ocean is regarded as the second very serious ecological consequence of the increasing accumulation of CO2 in the atmosphere
Coral reefs have exceptional biodiversity, and are now threatened by warmer oceans as well as acidification.
Ocean acidification is a change in sea water chemistry; CO2 reacts with water molecules (H2O) and forms the weak acid H2CO3 (carbonic acid). It is estimated that if CO2 continues to be released at the same rate as today, ocean acidity will increase by 170% compared to pre-industrial levels. The changes are happening at least 10 times faster than at any moment in the geological past. IAEA
The Monaco Declaration is an internationally, scientifically coordinated response to the ocean acidification problem: Monaco Declaration and Research Priorities Report Released
- 26%: The increase in ocean acidity from preindustrial levels to today.
- about 170%: The projected increase in ocean acidity by 2100 compared with preindustrial levels if high CO2 emissions continue .
- 10 times: The current rate of acidification is over 10 times faster than any time in the last 55 million years.
- 24 million: The number of tonnes of CO2 the ocean absorbs every day.
Ocean acidification 2014
Google Earth ocean acidification (2012)
A Google Earth tour explores the phenomenon of ocean acidification and explains why even small changes to ocean chemistry could have profound implications for marine life and future economic activities
Ocean Acidification – state of knowledge
World Bank, 2014, by dr Carol Turley from Plymouth Marine Laboratory (UK) summarises the current state of knowledge on Ocean Acidification.
The ocean absorbs almost half of the carbon dioxide emitted by human activities, changing its chemistry in ways that may have significant effects on marine ecosystems. Join Scripps marine chemist Andrew Dickson as he explains what we know — and what we don’t — about this emerging problem.
The oceans are changing. The Arctic oceans are warming, and turning more acid. Plankton at the base of the ecosystem are negatively affected and may harm productivity
NOAA Ocean Acidification – The Other Carbon Dioxide Problem
Fundamental changes in seawater chemistry are occurring throughout the world’s oceans. Since the beginning of the industrial revolution, the release of carbon dioxide (CO2) from humankind’s industrial and agricultural activities has increased the amount of CO2 in the atmosphere. The ocean absorbs almost a third of the CO2 we release into the atmosphere every year, so as atmospheric CO2 levels increase, so do the levels in the ocean. Initially, many scientists focused on the benefits of the ocean removing this greenhouse gas from the atmosphere. However, decades of ocean observations now show that there is also a downside — the CO2 absorbed by the ocean is changing the chemistry of the seawater, a process called ocean acidification. This change in the ocean’s chemistry will have profound effects on life in the ocean, and those who depend on it.
Ocean acidity may have increased as much as 30% the last hundred years.
- Ocean acidification (Skeptical science)
- Ocean acidification – CO2 putting shelled animals at risk (National Geographic)
- Coral reefs heading for fishing and climate crisis (BBC)
- Ocean Acidification Threatens Food Webs(National Geographic)
- The Acid Ocean – the Other Problem with CO2 Emission
- Ocean Acidification from CO2 Is Happening Faster Than Thought (Scientific American)
- Ocean acidification – the other CO2 problem
- The ocean in a high CO2 world
- Greening the blue
- Scientist Accuses The Times Newspaper of “Cherry Picking” on Ocean Acidification Story (2016)
- West Coast Ocean Acidification and Hypoxia (OAH) Science Panel
- World’s Reefs Caught Up in the Longest Global Coral Bleaching Event Ever Recorded (Jan 2017)
- Nature (2017) Rapid emergence of climate change in environmental drivers of marine ecosystems
- As coral reefs die, huge swaths of the seafloor are deteriorating along with them (April 2017)
Reduced oxygen production
|Home||Chapter 3||3. Impacts|
|3.1 More water vapor|
|3.2 Sea level rise|
|3.3 Polar sea ice|
|3.4 Air pollution|
|3.7 Extreme weather|
|3.9 Refugees and conflicts|
|3.11 Tipping points|
|Chapter 4||4. Ecosystems|