You may want to share this article with the various groups. Among the many issues it raises is the cause of the change of circumpolar winds in the Antarctic which could be a result of a change in the temperature gradient of the SH. The change in circumpolar winds maybe driving the observed changes to major Antarctic glaciers. No on I know has analysed how and if SRM might reverse this potentially devastating change in the circumpolar winds.
When scientists tagged a curious seal, he led them to signs of a potential climate disaster
The seal and robot helped scientists find a climate change disaster waiting to happen in one of the most mysterious regions on Earth: vast glaciers in West Antarctica.
By Chris Mooney and Simon Ducroquet
https://www.washingtonpost.com/climate-environment/2023/01/18/climate-change-glacier-antarctica/
Download The Washington Post app.
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From: Rafe Pomerance <rafe.po...@gmail.com>
Date: January 24, 2023 at 7:35:46 PM EST
To: rafe Pomerance <rafe.po...@gmail.com>
Subject: [The Washington Post] When scientists tagged a curious seal, he led them to signs of a potential climate disaster
Thwaites summaryI did chat with a Thwaites specialist today and confirmed that changes in the SH temperature gradient and resulting changes in circumpolar winds are an important component of what is happening in West Antartica, and in particular with Thwaites Glacier. The changes in both the air temperature gradient and the circumpolar wind intensity which are driving changes in warm water delivery to the base of deep Antarctic glaciers appear to be driven by our warming planet. So the question could be, can the air temperature gradient and circumpolar winds be returned to an earlier condition by either reducing net insolation energy or reducing greenhouse gas concentrations ? And, would that change the rate at which warmer deep water is interacting with Antarctic glaciers? My sense is that some of the experts think this is the case.
Just to note that warming in polar regions is greater than lower latitudes in part because virtually none of the trapped energy is going into evaporation because it is so cold, so virtually all goes into heating.. At low latitudes, much of the energy goes into evaporation and much less into heating--the payback being, of course, that the heat/discomfort index amplifies the impact of the temperature increase and the more the evaporation, the more (intense) precipitation.
Mike MacCracken
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On Jan 23, 2023, at 8:06 PM, Aaron Franklin <stateoft...@gmail.com> wrote:
Ok, this presentation from Scientists on how Arctic amplification and Global climate change is NOT caused by Anthropogenic Greenhouse gases, but Submarine Vulcanism is a must watch:I would suggest that you recognize that the Scientists who are measuring Salinities and temperatures of waters coming out from these glacial systems are being provided with sensors that "operate in quality controlled mode" this means they are deleting data that is too saline or hot to be seawater before anyone gets to see it.It is Subglacial volcanism and hydrothermal output driving the melt. Despite what certain agencies might want you to believe.RegardsAaron Franklin
On Tue, 24 Jan 2023, 12:26 pm Aria Mckenna, <ar...@globalcoolingproductions.com> wrote:
Thank you Rafe. I certainly look forward to hearing your take aways from from your conversation regarding Thwaites. 🙏🌎💦Warmest Thanks For Everything You Do,
🙏❤🌎🌾🐋💫
Aria McKenna
Creative Producer, Actress and Climate Communicator
718-288-0472
BECOMING THE CHANGE
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On Mon, Jan 23, 2023, 3:40 PM Rafe Pomerance <rafe.po...@gmail.com> wrote:
John, It may be the the temperature gradient shift in the SH is the reverse of the Arctic. The tropics are warming more than the polar region growing rather than shrinking the temperature gradient. Of course I might have this wrong, but that’s what I remember from earlier conversations with scientists. I am having a conversation with a key Thwaites scientist tomorrow and will review my understanding.Rafe
Rafe
On Jan 23, 2023, at 2:47 PM, John Nissen <johnnis...@gmail.com> wrote:
Cheers, JohnThanks Rafe,The West Antarctic glaciers are of concern. This disruption in East Antarctica could be an added reason to cool both poles. If the pole to tropics gradient has reduced in the Antarctic as well as the Arctic, then cooling the Antarctic would strengthen the circumpolar winds.
On Sun, Jan 22, 2023 at 10:37 PM Rafe Pomerance <rafe.po...@gmail.com> wrote:
You may want to share this article with the various groups. Among the many issues it raises is the cause of the change of circumpolar winds in the Antarctic which could be a result of a change in the temperature gradient of the SH. The change in circumpolar winds maybe driving the observed changes to major Antarctic glaciers. No on I know has analysed how and if SRM might reverse this potentially devastating change in the circumpolar winds.
When scientists tagged a curious seal, he led them to signs of a potential climate disaster
The seal and robot helped scientists find a climate change disaster waiting to happen in one of the most mysterious regions on Earth: vast glaciers in West Antarctica.
By Chris Mooney and Simon Ducroquet
https://www.washingtonpost.com/climate-environment/2023/01/18/climate-change-glacier-antarctica/
Download The Washington Post app.
------Sent from my iPhone
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Hi Rafe,
It would be interesting to know whether the Antarctic is warming slower than the tropics or whether there’s amplification going on. The NH westerlies are weakened as a result of Arctic Amplification (causing a sea level rise on the east coast of the USA); but the SH westerlies are strengthening [1].
Cheers, John
[1] BAS (2018)
Increases in westerly winds weaken the Southern Ocean carbon sink
https://phys.org/news/2018-07-westerly-weaken-southern-ocean-carbon.html
A new study of lake sediments from the sub-Antarctic reveals for the first time that increases in westerly winds are likely to reduce the ability of the Southern Ocean to absorb carbon dioxide from the atmosphere. The results are significant as the Southern Ocean currently absorbs over 40% of human-produced carbon dioxide, so any weakening of this 'carbon sink' could accelerate climate change. The findings are published today (Monday 23 July 2018) in the journal Nature Geoscience.
The Southern Hemisphere westerly winds (known by latitude as the roaring forties, furious fifties, and screaming sixties) are particularly strong due to the absence of continental landmasses between South America and Antarctica to slow them down. They play an important role in regulating how much carbon dioxide (greenhouse gas) is exchanged between the atmosphere and ocean. They do this by controlling the rate of mixing and upwelling of old carbon-rich deep water, which in turn determines how much carbon can be absorbed at the ocean surface. In the last few decades, there has been a strengthening of the westerly winds, and climate modellers have been unable to agree on whether this will enhance or weaken the Southern Ocean 'carbon sink'.
An international team of scientists measured the accumulation rate of wind-blown sea salts and minerals in a 12,000 year-old lake sediment record from sub Antarctic Macquarie Island. They show that periods of higher wind intensity directly correspond with periods of increasing atmospheric carbon dioxide measured in ice cores. This suggests that further increases in wind strength may well reduce the capacity of the Southern Ocean 'carbon sink'.