IPCC AR6 Synthesis Report: Key Cryosphere Related Takeaways
The IPCC finalised the Synthesis Report for the Sixth Assessment Report
during the Panel's 58th Session held in Interlaken, Switzerland during
March 13-19, 2023. The report highlights that the global surface temperature
has increased by 1.1°C in the last decade, and explains the implications of
this rise in the Cryosphere along with its implications on people and
ecosystems. The report predicts that drastic reductions in the greenhouse gas
emissions can only restrict disastrous changes post 2050 but advises
context-based adaptation and transformative governance to reduce the associated
risks of climate change to a great extent.
The Intergovernmental Panel on Climate Change (IPCC) 6th Assessment
Resource (AR6) Synthesis Report has revealed that the global surface
temperature has increased by 1.1°C during 2011-2020, as compared to 1850-1900
levels (Intergovernmental Panel on Climate Change, 2023). The Paris
Agreement outlined in Conference of the Parties (CoP) 21 presented a
sustainable path by taking up the target to limit the rise in temperature to
1.5°C by the end of this century. Greenhouse gases, majorly contributed by
human activities are the majorly responsible for this increase and as per the
report the major sources are fossil fuels, industrial processes, urban systems,
transportation, and agricultural emissions, etc.
Out of the total cumulative net CO₂ emissions since 1850, 42 per
cent of the emissions were contributed during 1990-2019. The recent rise in
temperature has had negative impacts on the atmosphere, ocean, cryosphere,
biosphere, weather, ecosystems, amongst others and it is the vulnerable
communities, who in all the ecosystems, are at the receiving ends of disastrous
consequences of this climate change. For instance, the mortalities from droughts,
storms, floods were almost 15 times more in the vulnerable regions as compared
to other regions during 2010-2020. This highlights the significance of the
principle of ‘Climate Equity’ in the discourse of climate change. The other
implications of climate change faced by the world include a rise in sea level
on an average of 3.7 mm per year (2006-2018); ocean warming; climate extremes,
namely heatwave, erratic precipitation, cyclones, cold waves; impact on
hydrology due to glacial and ice-sheet retreat in mountains, Polar ecosystems;
water scarcity (almost 50 per cent of world’s population faces the threat of
severe water scarcity) agricultural and health crisis; food insecurity and many
more. Adaptation and mitigation may act as resolves to the issue of climate
change. However, adaptation gaps, contextual limitations to adaptation,
maladaptation, insufficient financial flows, technology deficits, insufficient
research and political will, and lack of citizen engagement are becoming
reasons for not only abrupt but also irreversible changes that might bring many
systems on the verge of collapse.
IPCC Findings on Impact of Climate Change in Cryosphere
Current Status
Each and every being on the earth is directly or indirectly connected to
the well-being of oceans and cryosphere. In the Special Report on the
Ocean and Cryosphere in a Changing Climate, a part of IPCC 6th Assessment
cycle, cryosphere is defined as the ‘components of the Earth System at and
below the land and ocean surface that are frozen, including snow cover,
glaciers, ice sheets, ice shelves, icebergs, sea ice, lake ice, river ice,
permafrost, and seasonally frozen ground’. Global warming has led to the shrinking
of the cryosphere to a large extent in the last decade. There has been a
significant impact such as loss in the thickness of ice sheets, glaciers, snow
covers; rise in permafrost thawing; extinction of Arctic sea ice. From
2006-2015, the Antarctic Icesheets has lost the ice mass at the rate of 155
± 19 Gt per year. A rise in surface air temperature leading to surface
melting has been causing these losses majorly. In almost all the high mountain
regions including the Himalaya, the snow cover and glacial extents have been
facing declines in recent decades. The trend of rise in Permafrost temperatures
has been at record levels across the polar and high mountain areas since the
1980s. For instance, the quantity of organic carbon has reached to 1,460-1,600
Gt in Arctic and boreal permafrost which is double the amount of atmospheric
carbon.
Implications of Climate Change on People and Ecosystems
Glacial retreat, melting of Greenland and Antarctic ice sheet and
thermal expansion has been leading to an acceleration in the rise of Global
Mean Sea Level (GMSL). As per the report from 2006-2015, ice sheets and glacier
melt have been acting as the significant source of sea level rise of 1.8 mm per
year and anthropogenic forcing is the dominant cause for it since 1970. This
has also led to an increase in extreme sea level events causing coastal hazards
such as cyclones, extreme waves, storm surges. Wildfires, permafrost thaws,
impact on mountain ecology are the pertinent issues that cryospheric regions
have been facing. Coastal ecosystems such as coastal wetlands provide
protection to coastlines from impending disasters such as sea level rise,
change in weather patterns along with being carbon sinks. However, in the past
hundred years, almost 50 per cent of wetlands have been lost releasing
0.04-1.46 Gt of carbon per year. Change in cryosphere has also led to a change
in hydrology, engendering the phenomenon of plant and animals’ species shift.
Recent examples of change in the seasonal and production behavior of certain
Arctic zooplanktons and shift in the spread of Antarctic krill in the Southern
Atlantic demonstrate the phenomenon of species shift due to change in climatic
dynamics. The report highlights that the rate of poleward shift of certain
marine species since the 1950s has been around 52 ± 33 km per decade.
This affects the whole food web, ecosystem, and biodiversity altogether.
Cryospheric shrinking in Polar Regions like Arctic, Himalayas has
brought with itself several other negative externalities such as food
insecurity, water scarcity, health issues, threat to indigenous communities,
infrastructural issues, etc. For instance in the Himalaya, a retreat in glacier
and snow cover has led to a reduction in agricultural yields. In terms of
impacts on health, change in cryosphere also leads to rise in the risk related
to food and water-borne diseases compounding the severity of issues such as
malnutrition, psychological challenges, water scarcity, amongst others.
Indigenous communities remain most vulnerable to these risks. Even the
adaptation at the infrastructural level for resilience has been facing the
problem of funding, skilling, institutional support, etc. Along with this the
opening of new routes in cryospheric regions due to thawing of sea ice does not
only open up the new frontiers for geopolitics but also poses risks such as
fear of introduction of invasive species, pollution, threat to marine
ecosystems, etc. Similarly, due to changes in hydrological systems, hydropower
systems face imminent threats due to variability in availability of water and
linked disasters such as Glacial lake outburst that threaten the
hydropower projects at downstream (Chandrashekhar, 2022).The report also
mentions that Glacial and snow cover retreat has impacted the high mountain
aesthetics and culture negatively.
Future Predictions and Associated Risks
With the current rate of increase in surface air temperature, decline in
snow, sea ice cover, glacial retreat and permafrost thaw would continue to be
the predominant leading to many possible hazards and change in river
ecosystems. Smaller glaciers are projected to lose 80 per cent of their ice
mass by 2100 in the scenario of rapid emissions. If the emissions continue to
increase with this rate, near 70 per cent of surface level permafrost could be
lost by 2100. It could even lead to irreversible ice-sheet instability in the
polar regions. Antarctic sea ice is predicted to be the largest contributor to
sea level rise by the end of 21st century. Similarly, 20 per
cent of land in the Arctic faces the threat of abrupt permafrost thaw with
associated risks such as ground subsidence, drying up of soil, wildfires, etc.
The severity of other imminent threats such as instability of slopes, number of
glacial lakes and floods due to their breach, landslides, snow avalanches,
increase in coastal waves and tidal amplitude, species shifting, loss to
biodiversity, and other extreme sea level events may be increased.
The Special Interest Problem
Consensus Building is one of the most critical aspects of effective climate action. The recently released IPCC AR6 Report was watered down from its original version as the Report Summary for policymakers needs the unanimous buy-in from delegates of all 195 nations, thus, giving a chance to policymakers to pursue intense negotiations (Inside Climate News, 2023). However, climate negotiations can be challenging due to the involvement of different political and financial interests of the countries. Representatives from several countries negotiated ferociously to remove or water down specific references, such as the grave environmental cost of fossil fuels and meat consumption. For instance, Brazil and Argentina got the negative effect of the consumption of meat on the environment removed successfully.
Way Forward
Although the report predicts that drastic changes in
the greenhouse gas emissions can only restrict disastrous changes post 2050.
Incremental steps such as context-based adaptation and transformative
governance can reduce the risk to a great extent. Slowing of the rate of
cryosphere change is much desired as it can extend the window of opportunity to
take resilient and effective actions to reverse the trajectory of climate
change. Countries within the framework of international cooperation must act to
fulfill their commitments under Intended Nationally Determined Contributions,
taken up by the countries in the Paris Agreement under the United Nations
Framework Convention on Climate Change (UNFCCC). The report also underlines
that those countries and people who are least capable to respond are those that
are highly exposed and vulnerable. In this scenario, the resolve on climate
financing from the developed world must be fulfilled and adherence to the
promises under Green Climate Fund should be non-negotiable. Along with
financial flows, there should also be a development of reliable technologies
that can facilitate the transition of the least developed and developing
countries towards cost-effective adaptation and mitigation measures, fulfilling
the ambition of the world to limit the rise in temperature to 1.5° C by
the end of this century.
References
Chandrashekhar, V. (2022). How climate change
is threatening Himalayan hydropower projects:https://timesofindia.
Intergovernmental Panel on Climate Change
(2023). Synthesis Report of the IPCC Sixth Assessment Report (AR6).
Intergovernmental Panel on Climate Change.
(2019). The Ocean and Cryosphere in a Changing Climate.
Inside Climate News . (2023, March 28). Corporate
Interests ‘Watered Down’ the Latest IPCC
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