With a lot of debate this week on how models simulate permafrost thaw & climate impacts, I want to explain how we actually MEASURE permafrost change. Follow this thread for the pretty scenes or the weird science. Here is me caught in a surprise ❄️ squall w/ permafrost gear. 1/
The traditional method of monitoring permafrost change is through the trusty frost probe. In this quick video I explain our work on 🔥-permafrost interactions while taking a frost probe measurement. 2/
Below check out a time lapse video of frost probing along one of our transects in the Northwest Territories 🇨🇦. I share these field sites with an array of incredible students & the fabulous @forestecogrp. 3/
Frost probing tells us whether the top active layer is thickening & thus thawing surface permafrost. But what about carbon? Well one approach is to frost probe near collars where we measure CO2 & CH4 emissions. Here @fen_fatale probes our @BNZ_LTER flux collars near Fairbanks. 4/
Another challenge for us is to quantify how much carbon is contained in the permafrost & how this varies w/ depth. We can drill into the frozen soils w/ some elbow grease & mechanical help. We can collect a few meters of core this way, bigger drill rigs can go much deeper! 5/
Images of permafrost cores! Notice the variation in color & patterns. Permafrost can be frozen peat or mineral soil. Frozen peat tends to be very carbon-rich! We collect & analyze these cores before & after 🔥. Another measure of permafrost change! 6/
After thaw of ice-rich permafrost, soils are so wet that we use limnology methods to collect them. The frozen finger technique uses dry ice to freeze thawed material to the outside of our corer. This is weird science for sure! @CarolynG_22@subarcticmonkee 7/
Here @CarolynG_22 explains the method w/ @subarcticmonkee. Notice the 🦟 flying around even though this was late in the season. 8/
@MiriamCJones@kmanies & I took yrs to develop this method for saturated thawed permafrost soils. Here is the end result - previously frozen permafrost organic matter "stuck" to the outside of our cores, we can then sample it w/ depth & analyze carbon concentrations. @USGS 9/
Temperature monitoring of course is important for monitoring permafrost change. But to understand how thaw affects carbon, we need to make lots more measurements like the ones in this thread. I welcome my perma-peeps to chime in w/ their fav methods! The end & thanks! 10/10
• • •
Missing some Tweet in this thread? You can try to
force a refresh
@ClimateOfGavin@mammuthus@theresphysics Buckle up for a permafrost ride! This paper is a thought experiment that relies on my empirical & modeling work on permafrost C release. First, I ♥️ using models for thought experiments so that is a positive here. Below is what permafrost THAW looks like - it's complicated! 1/
@ClimateOfGavin@mammuthus@theresphysics Permafrost is represented very crudely in most models to date. We know these frozen soils store a lot of C, but we know that only a fraction of that C is vulnerable to decomposition post-THAW. As temp constraints are released, there are other mechanisms that protect that C. 2/
@ClimateOfGavin@mammuthus@theresphysics Only a fraction of permafrost C is vulnerable to release upon THAW, & of that most will be released as CO2. I study methane & yes it's important & likely to be more so in the future. The authors' thought experiment regarding fraction of methane release in this paper is silly. 3/
It's a great day for a permafrost mash-up! Let's combine a few things I love - permafrost, language, & culture. Follow this thread if you want to learn some *cool* words from across the Arctic. Great for Scrabble or your next northern adventure. My top 10 #Permaterms 1/
My first #permaterm is pingo, which means small hill in Inuvialuit. A pingo is a mound in the permafrost region that has a core of massive ice & covered w/ soil & vegetation. Several are protected in the Pingo National Landmark area,Tuktoyaktuk Northwest Terroritories Canada. 2/
Pingos vary in size & can have a crater that form as the surface ruptures during doming. The term pingo has been part of western science lexicon since the 1930’s (attributed to botanist Alf Porsild) & today is preferred over the older technical term hydrolaccolith. 3/
Welcome to my dive into #MarvelousMoss. Most of what we know about plants centers on vascular plants. But there is this incredibly rich & interesting lineage(s) of nonvascular plants or bryophytes. These plants are other-worldly, create habitat & be habitat, & defy physics! 1/
Bryophytes=liverworts, hornworts, mosses are often referred to as cryptogams (meaning hidden reproduction). But I think about cryptic diversity. Most of the plant diversity in northern ecosystems is on the ground, difficult to ID, but provides loads of important functions. 2/
Time for a deep time dive! Mosses are the closest relatives to the first land plants. The first bryophytes emerged in the Cambrian (aka Cambrian explosion of diversification) while the living clade of vascular plants emerged later in the Ordovician. 3/ pnas.org/content/115/10…
🔥is now shaping the Arctic. In @NatureGeosci
we outline a call to action. Key messages - 1) a global climate problem requires a global scale solution, 2) western science can't tackle this without Indigenous knowlege holders. w/ @jmccarty_geo@DrTELSinstaar.colorado.edu/news-events/in…
2/ Will Arctic 🔥 burn into ancient carbon stored in peat & permafrost? We conclude that the 2020 fires in Siberia showed signs of holdover or zombie fires, which can overwinter in deep peat & influence burning the following season. This represents momentum in the climate system.
3/ Scientists have long debated the use of the term zombie fire, but also the importance of these holdover conditions. How important are they? Moving from anecdotal to monitoring will require collaborating with local knowledge holders. ilinationhood.ca/our-work/guard…
Stay tuned for my top 10 facts about #BadAssBogs! Bogs are weird, logistically challenging & sometimes smelly. But they have fascinating plants, are an archeology & paleoecology resource, & are one of the most efficient stockpiles of carbon in the biosphere. What's not to ♥️?
BogFact 1: Did you know that bogs breathe? The bog surface shrinks & expands as the water table moves up & down. This is a great example of the ecohydrology that makes bogs so unique. The traits of bog plants & soil reinforce the bog sponge -it's adaptive! link.springer.com/article/10.100…
BogFact 2: Bogs are actually quite rare. These are ombrotrophic systems. Ombros=rain; trophic=fed. Scientists gravitate towards bogs because they are closed systems and relative easy to study. But in 🇨🇦 bogs are <10% of peatland cover. Fens (surface & ground water fed) rule!
Recently I was invited to help revise a classic #limnology book. Editors say they care about diversity but have no plan & are evading the issue. From @ElsevierConnect@ElsevierNews: "We can identify issues that impede inclusion in science and take action to resolve them." 1/
We need to do more than talk about diversity, justice, & equity. Without action & accountability, the book will perpetuate our racism in #ecology. I raised the issue twice & walked away frustrated, but I am curious to hear from others. Is there more I should have done? 2/
My question for @ElsevierConnect@ElsevierNews, what is your equity & diversity policy for contributed book projects? The policies I found are mostly internal or program-based. What are you doing to break racist cycles in what you produce- your legacy- & send into the world? 3/3