APP Users: If unable to download, please re-install our APP.
Only logged in User can create notes
Only logged in User can create notes

General Studies 3 >> Enivornment & Ecology

audio may take few seconds to load

Stockholm+50

                     STOCKHOLM +50 - OCEANS ON SIMMER

 
KEY POINTS :
  • Oceans regulate the climate by absorbing atmospheric carbon dioxide and by altering the energy budget, carbon cycle and nutrient cycle.
  • Oceans reduce the worst impacts of climate change by absorbing 90% of excess global temperature rise and 25% of COemissions.
  • Global warming is causing warming, acidification and deoxygenation of oceans.
  • The oceans have warmed unabated since 2005, continuing the clear multi-decades trends documented by the Intergovernmental Panel on Climate Change(IPCC).
  • The temperature on the ocean surface has increased by 0.88o C from 1850-1900 to 2011-20, with 0.60o C of the warming occurring since 1980.
  • The ocean temperature is projected to increase by about 1.5 C by 2050, not only on surface waters but also in deep ocean waters.
  • The major impact of ocean warming is seen over the Arctic Ocean which will likely become sea ice-free during the sea ice minimum for the first time before 2050.
  • It is virtually certain that the global mean sea level 0.18-0.23m by 2050 and 0.38-0.77m by 2100.
  • This rise in sea level is mainly due to thermal expansion and mass loss from glaciers and ice sheets.
  • Unlike atmospheric heatwaves, MHW(Marine Heat Waves) can extend millions of square kilometres and persist for weeks to months.
  • MHW can lead to severe and persistent impacts on marine ecosystems, coral bleaching, changes in phytoplankton blooms, shifts in species composition and toxic algal blooms.
  • The IPCC climate change projections suggest that MHWs will become four times more frequently by 2080 compared to the 1995-2011 threshold.
  • The rate of ocean uptake of atmospheric CO2 has continued to strengthen in response to the rising atmospheric CO2.
  • The open ocean surface water pH is observed to be declining by 0.017-0.027 pH units since the 1980s.
  • There is a growing consensus that the open ocean is losing oxygen, with a likely loss of 0.5-3.3% between 1970-2010 from the ocean surface to 1000m.
  • The oxygen minimizing zones are expanding by 2-8%, most notable in the tropical oceans.
MARINE ECOSYSTEM HIT-
  • The warming of oceans has serious adverse impacts. Global warming can fundamentally alter ocean biodiversity.
  • It affects the marine organisms at multiple levels, impacting fisheries, and food production.
  • 'The Global Assessment Report on Biodiversity and Ecosystem Services' finds that 66% of the global ocean is impacted by human pressures, with severe impacts in the declining richness and abundance of ocean biodiversity.
  • There is high confidence in inferring that fisheries, catches and their composition in many regions that are already impacted.
  • The erosion of ocean biodiversity and ecosystems particularly threatens the livelihoods of local communities.
COASTAL STRESS-
  • Coastal ecosystems are observed to be under stress from ocean warming and sea-level rise that are exacerbated by non-climatic pressures from human activities on the ocean and land.
  • The global wetland area has declined by nearly 50% relative to the pre-industrial level.
  • Warming related mangrove encroachment into subtropical salt marshes was seen in the past 50 years.
  • The occurrence of algal blooms and pathogenic organisms has increased in coastal areas due to warming, deoxygenation and eutrophication with negative impacts on food provisioning, tourism, economy and human health.
EXTREME EVENTS-
  • A tropical cyclone(CT) is the most important weather system, which ocean warming can influence.
  • An increase in sea surface temperatures and ocean heat content could help TCs intensify quickly and travel long distances without losing appreciable energy.
  • Studies have suggested that there is a 6% increase in TC exceedance probability of 50.
  • The climate change projections suggest that average peak TC wind speeds & the proportion of very severe TCs will be increased with global warming.
  • The average locations where TCs reach their peak wind intensity will migrate poleward as the tropics expand with warming.
  • The Indian Ocean is also warming and the trend is likely to continue.
  • The warm Indian Ocean can lead to more intense precipitation events over India during the monsoon, as it will help to more moisture advection.
MITIGATION WAYS-
  • In view of the projected adverse impacts of warming oceans, there is a concern about the efficacy of ocean governance, highlighting the need for timely mitigation and adaptation responses.
  • There are three major risks-  i) the impacts of the over-exploitation of marine resources, ii) inequitable distribution of access to and benefits from marine ecosystem services, and iii) inadequate adaptation to changing ocean conditions.
  • The actions that can reduce this risk are related to the process of co-creation and implementation of improved, comprehensive and integrated ocean management and enhancement of the decision-making process.
  • The 2030 Agenda for Sustainable Development, adopted by all UN member states, provides a blueprint for peace and prosperity for the planet.
  • There are 17 Sustainable Development Goals(SDG) which are an urgent call for action.
  • SDG 14 is to conserve and sustainably use the oceans, seas and marine resources for sustainable development.
  • The UN has proclaimed a Decade of Ocean Science for Sustainable Development (2021-2030) to support efforts, and ensure ocean science can help countries to create improved conditions for sustainable development of the ocean. 

Share to Social