Sea-level rise - Revision history

Designing Buildings: Protected "Sea-level rise" ([edit=sysop] (indefinite) [move=sysop] (indefinite))

2022-09-03T16:53:30Z

Protected "Sea-level rise" ([edit=sysop] (indefinite) [move=sysop] (indefinite))

← Older revision

Revision as of 16:53, 3 September 2022

Designing Buildings at 06:07, 2 September 2022

2022-09-02T06:07:16Z

← Older revision		Revision as of 06:07, 2 September 2022
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−	[[File:~~Sea Level Europe~~.png\|link=https://www.eea.europa.eu/ims/global-and-european-sea-level-rise]]	+	[[File:Sea_Level_Europe.png\|link=https://www.eea.europa.eu/ims/global-and-european-sea-level-rise]]

−	~~In 2022,~~ August 29 the paper [https://www.nature.com/articles/s41558-022-01441-2 'Greenland ice sheet climate disequilibrium and committed sea-level rise'] published in nature climate change We found that the Greenland ice imbalance ~~with the recent (2000–2019) climate~~ commits at least 274 ± 68 mm Sea-Level Rise (SLR) from 59 ± 15 × 103 km2 ice retreat, equivalent to 3.3 ± 0.9% volume loss, regardless of twenty-first-century climate pathways. In simple terms indicating that a minimum of 27cm of global sea level rise is likely irrespective of climate action.	+	On August 29 2022, the paper [https://www.nature.com/articles/s41558-022-01441-2 'Greenland ice sheet climate disequilibrium and committed sea-level rise'] was published in nature climate change. It found that the Greenland ice imbalance commits us to at least 274 ± 68 mm Sea-Level Rise (SLR) from 59 ± 15 × 103 km2 ice retreat, equivalent to a 3.3 ± 0.9% volume loss, regardless of twenty-first-century climate pathways. In simple terms indicating that a minimum of 27cm of global sea level rise is likely irrespective of climate action.

−	In 2021 The Proceedings of the National Academy of Sciences (PNAS) published a paper entitled [https://www.pnas.org/doi/full/10.1073/pnas.2024192118 'Critical slowing down suggests that the western Greenland Ice Sheet is close to a tipping point'] indicating that in response to anthropogenic global warming a crucial nonlinear mechanism or positive melt-elevation feedback will create a tipping point ~~western~~ for the Greenland Ice Sheet. This feedback occurs where melting reduces the height of an ice sheet, in turn exposing the ice sheet surface to warmer temperatures, which further accelerates melting.	+	In 2021 The Proceedings of the National Academy of Sciences (PNAS) published a paper entitled [https://www.pnas.org/doi/full/10.1073/pnas.2024192118 'Critical slowing down suggests that the western Greenland Ice Sheet is close to a tipping point'] indicating that in response to anthropogenic global warming a crucial nonlinear mechanism or positive melt-elevation feedback will create a tipping point for the Greenland Ice Sheet. This feedback occurs where melting reduces the height of an ice sheet, in turn exposing the ice sheet surface to warmer temperatures, which further accelerates melting.

	In [https://www.climate.gov/news-features/featured-images/greenland-ice-loss-2020-was-below-record-above-average 2020 a report based on the Arctic Report Card (ARC)], showed that between September 2018 and August 2019, the Greenland Ice Sheet set a record for ice loss (532 ± 58 billion metric tons). Between September 2019 and August 2020, the rate of ice loss from the Greenland Ice Sheet was much lower (293 ± 66 billion metric tons), but still above the 2002–2020 average measured by GRACE. Average ice loss for Greenland over the full 18-year record was 268 ± 14 billion metric tons per year.		In [https://www.climate.gov/news-features/featured-images/greenland-ice-loss-2020-was-below-record-above-average 2020 a report based on the Arctic Report Card (ARC)], showed that between September 2018 and August 2019, the Greenland Ice Sheet set a record for ice loss (532 ± 58 billion metric tons). Between September 2019 and August 2020, the rate of ice loss from the Greenland Ice Sheet was much lower (293 ± 66 billion metric tons), but still above the 2002–2020 average measured by GRACE. Average ice loss for Greenland over the full 18-year record was 268 ± 14 billion metric tons per year.
−
−	[https://www.historicenvironment.scot/archives-and-research/publications/publication/?publicationId=843d0c97-d3f4-4510-acd3-aadf0118bf82 A Guide To Climate Change Impacts, On Scotland’s Historic Environment], published by Historic Environment Scotland in October 2019, defines sea-level rise as: ‘A hazard that contributes to issues such as coastal erosion and coastal flooding.

	= Related articles on Designing Buildings =		= Related articles on Designing Buildings =

Editor at 08:17, 30 August 2022

2022-08-30T08:17:02Z

← Older revision		Revision as of 08:17, 30 August 2022
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		+	[[File:Sea Level Europe.png\|link=https://www.eea.europa.eu/ims/global-and-european-sea-level-rise]]
		+
	In 2022, August 29 the paper [https://www.nature.com/articles/s41558-022-01441-2 'Greenland ice sheet climate disequilibrium and committed sea-level rise'] published in nature climate change We found that the Greenland ice imbalance with the recent (2000–2019) climate commits at least 274 ± 68 mm Sea-Level Rise (SLR) from 59 ± 15 × 103 km2 ice retreat, equivalent to 3.3 ± 0.9% volume loss, regardless of twenty-first-century climate pathways. In simple terms indicating that a minimum of 27cm of global sea level rise is likely irrespective of climate action.		In 2022, August 29 the paper [https://www.nature.com/articles/s41558-022-01441-2 'Greenland ice sheet climate disequilibrium and committed sea-level rise'] published in nature climate change We found that the Greenland ice imbalance with the recent (2000–2019) climate commits at least 274 ± 68 mm Sea-Level Rise (SLR) from 59 ± 15 × 103 km2 ice retreat, equivalent to 3.3 ± 0.9% volume loss, regardless of twenty-first-century climate pathways. In simple terms indicating that a minimum of 27cm of global sea level rise is likely irrespective of climate action.

Editor at 08:08, 30 August 2022

2022-08-30T08:08:12Z

← Older revision		Revision as of 08:08, 30 August 2022
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		+	In 2022, August 29 the paper [https://www.nature.com/articles/s41558-022-01441-2 'Greenland ice sheet climate disequilibrium and committed sea-level rise'] published in nature climate change We found that the Greenland ice imbalance with the recent (2000–2019) climate commits at least 274 ± 68 mm Sea-Level Rise (SLR) from 59 ± 15 × 103 km2 ice retreat, equivalent to 3.3 ± 0.9% volume loss, regardless of twenty-first-century climate pathways. In simple terms indicating that a minimum of 27cm of global sea level rise is likely irrespective of climate action.
		+
		+	In 2021 The Proceedings of the National Academy of Sciences (PNAS) published a paper entitled [https://www.pnas.org/doi/full/10.1073/pnas.2024192118 'Critical slowing down suggests that the western Greenland Ice Sheet is close to a tipping point'] indicating that in response to anthropogenic global warming a crucial nonlinear mechanism or positive melt-elevation feedback will create a tipping point western for the Greenland Ice Sheet. This feedback occurs where melting reduces the height of an ice sheet, in turn exposing the ice sheet surface to warmer temperatures, which further accelerates melting.
		+
		+	In [https://www.climate.gov/news-features/featured-images/greenland-ice-loss-2020-was-below-record-above-average 2020 a report based on the Arctic Report Card (ARC)], showed that between September 2018 and August 2019, the Greenland Ice Sheet set a record for ice loss (532 ± 58 billion metric tons). Between September 2019 and August 2020, the rate of ice loss from the Greenland Ice Sheet was much lower (293 ± 66 billion metric tons), but still above the 2002–2020 average measured by GRACE. Average ice loss for Greenland over the full 18-year record was 268 ± 14 billion metric tons per year.
		+
	[https://www.historicenvironment.scot/archives-and-research/publications/publication/?publicationId=843d0c97-d3f4-4510-acd3-aadf0118bf82 A Guide To Climate Change Impacts, On Scotland’s Historic Environment], published by Historic Environment Scotland in October 2019, defines sea-level rise as: ‘A hazard that contributes to issues such as coastal erosion and coastal flooding.		[https://www.historicenvironment.scot/archives-and-research/publications/publication/?publicationId=843d0c97-d3f4-4510-acd3-aadf0118bf82 A Guide To Climate Change Impacts, On Scotland’s Historic Environment], published by Historic Environment Scotland in October 2019, defines sea-level rise as: ‘A hazard that contributes to issues such as coastal erosion and coastal flooding.

−	= Related articles on Designing Buildings ~~Wiki~~ =	+	= Related articles on Designing Buildings =

	* Carbon plan.		* Carbon plan.

Designing Buildings at 07:29, 18 May 2021

2021-05-18T07:29:28Z

← Older revision		Revision as of 07:29, 18 May 2021
Line 12:		Line 12:
	* Flood risk.		* Flood risk.
	* Flood.		* Flood.
		+	* Mean sea level.
	* Pitt Review Lessons learned from the 2007 floods.		* Pitt Review Lessons learned from the 2007 floods.
	* River engineering.		* River engineering.

Designing Buildings: Created page with "[https://www.historicenvironment.scot/archives-and-research/publications/publication/?publicationId=843d0c97-d3f4-4510-acd3-aadf0118bf82 A Guide To Climate Change Impacts, On Sco..."

2021-04-05T06:43:45Z

Created page with "[https://www.historicenvironment.scot/archives-and-research/publications/publication/?publicationId=843d0c97-d3f4-4510-acd3-aadf0118bf82 A Guide To Climate Change Impacts, On Sco..."

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[https://www.historicenvironment.scot/archives-and-research/publications/publication/?publicationId=843d0c97-d3f4-4510-acd3-aadf0118bf82 A Guide To Climate Change Impacts, On Scotland’s Historic Environment], published by Historic Environment Scotland in October 2019, defines sea-level rise as: ‘A hazard that contributes to issues such as coastal erosion and coastal flooding.

= Related articles on Designing Buildings Wiki =

* Carbon plan.
* Climate Change Act.
* Climate change.
* Coastal change management area
* Coastal defences
* Coastal erosion
* Coastal Transition Zone
* Flood risk.
* Flood.
* Pitt Review Lessons learned from the 2007 floods.
* River engineering.
* Water engineering.

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