The permafrost zone is expected to be a substantial carbon source to the atmosphere, yet large-scale models currently only simulate gradual changes in seasonally thawed soil. Abrupt thaw will probably occur in <20% of the permafrost zone but could affect half of permafrost carbon through collapsing ground, rapid erosion and landslides. Here, we synthesize the best available information and develop inventory models to simulate abrupt thaw impacts on permafrost carbon balance. Emissions across 2.5 million km2 of abrupt thaw could provide a similar climate feedback as gradual thaw emissions from the entire 18 million km2 permafrost region under the warming projection of Representative Concentration Pathway 8.5. While models forecast that gradual thaw may lead to net ecosystem carbon uptake under projections of Representative Concentration Pathway 4.5, abrupt thaw emissions are likely to offset this potential carbon sink. Active hillslope erosional features will occupy 3% of abrupt thaw terrain by 2300 but emit one-third of abrupt thaw carbon losses. Thaw lakes and wetlands are methane hot spots but their carbon release is partially offset by slowly regrowing vegetation. After considering abrupt thaw stabilization, lake drainage and soil carbon uptake by vegetation regrowth, we conclude that models considering only gradual permafrost thaw are substantially underestimating carbon emissions from thawing permafrost.
Good coverage by the Financial Times on the new study on the risk of Atlantic Ocean circulation instability, citing a number of experts. #AMOC
It’s a secret Cabinet document that has @CSIRO urging #ClimateActionNow to prevent catastrophic weather events and other serious adverse environmental effects from occurring. The only reason I have access to it is because it’s 34 years old. #auspolpic.twitter.com/Qu0dc6moB9
📈According to the #ERA5dataset, the 7 days from 3rd to 9th July 2023 were the 7 hottest days on record globally, making the first week of July 2023 the hottest week on record.
Thanks again for the detailed assessment @RARohde!
"An analysis suggests that removing the sulfate aerosols may have added ~0.2 °C (~0.4 °F) to the North Atlantic region. This would not explain all of the present North Atlantic spike, but may have added to its severity." https://t.co/vkZAaTzuDZpic.twitter.com/QkJTBtL5Bi
In Norway they tax the fossil fuel industry & give free university education to young people. In Australia we subsidise the fossil fuels & charge people a fortune to go to uni…decisions about taxing & spending are much more important than droning on about budget deficits #auspolpic.twitter.com/mkof2xFc4n
As reported by @WeatherProf, Manatee Bay, FL, recorded an astonishing sea surface temperature (SST) of 101.1°F (38.4°C) at a depth of 5' today, and also hit 100.2°F (37.9°C) yesterday — common hot tub temperatures! An SST of 101.1°F could be a world record. A 🧵 1/9 pic.twitter.com/r4uupDCsv7
The very hot sea surface temperatures (SST) in the North Atlantic roughly coincide with exceptionally weak winds in June, see https://t.co/5Cr6SsXHTJ. A contributing mechanism could be rather shallow wind-mixed surface layers of a few tens of meters, which heat up more quickly… pic.twitter.com/DMOvFVr0h2
— Prof. Stefan Rahmstorf 🌏 🦣 (@rahmstorf) July 13, 2023
Some call me a 'climate scientist'. I'm not. What I am is an 'Earth systems generalist'.
Born in 1939, I grew up with passionate interests in both science and engineering. I learned to read from my father's university textbooks in geology and paleontology, and dreamed of building nuclear powered starships. Living on a yacht in Southern California I grew up surrounded by (and often immersed in) marine and estuarine ecosystems while my father worked in the aerospace engineering industry.
After studying university physics for three years, dyslexia with numbers convinced me to change my focus to biology. I completed university as an evolutionary biologist (PhD Harvard, 1973). My principal research project involved understanding how species' genetic systems regulated the evolution and speciation of North America's largest and most widespread lizard genus. Then for several years as an academic biologist I taught a range of university subjects as diverse as systematics, biogeography, cytogenetics, comparative anatomy and marine biology.
In Australia, from 1980, I was involved in various activities around the emerging and rapidly evolving microcomputing technologies culminating in 2 years involvement in the computerization of the emerging Bank of Melbourne.
In 1990 I joined a startup engineering company that had just won the contract to build a new generation of 10 frigates for Australia and New Zealand. In 2007 I retired from the head office of Tenix Defence, then Australia's largest defence engineering contractor, after a 17½ year career as a documentation and knowledge management systems analyst and designer. At Tenix I reported to the R&D manager under the GM Engineering, and worked closely with support and systems engineers on the ANZAC Ship Project to solve documentation and engineering change management issues that risked the project 100s of millions of dollars in cost and years of schedule overruns. All 10 ships had been delivered on time, on budget to happy customers against the fixed-price and fixed schedule contract.
Before, during, and after these two main gigs I also did a lot of other things that contribute to my general understanding of complex dynamical systems involving multiple components with non-linear and sometimes chaotically interacting components; e.g., 'Earth systems'.
Earth's Climate System is the global heat engine driven by the transport and conversions of energy between the incoming solar radiation striking the planet, and the infrared radiation of heat away from the planet to the cold dark universe.
As Climate Sentinel News Editor, my task is to identify and understand quirks and problems in the operation of this complex heat engine that threaten human existence, and explain to our readers how they can help to solve some of the critical issues that are threatening their own existence.