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#firn — Public Fediverse posts

Live and recent posts from across the Fediverse tagged #firn, aggregated by home.social.

  1. Meeting LISA

    LISA: the Lightweight In Situ Analysis box is one of a kind, built by our friends at PICE in the Niels Bohr Institute. Later this year we're taking LISA to #Antarctica for the first time ever, to analyse shallow #snow and #firn cores directly in the field. We hope LISA will help us understand how much snow falls in Dronning Maud Land, how much it varies from year to year and what is the influence of sea ice and far field atmospheric processes on the rate…

    sternaparadisaea.net/2025/09/3

  2. Meeting LISA

    LISA: the Lightweight In Situ Analysis box is one of a kind; built by our friends at PICE in the Niels Bohr Institute. Later this year we’re taking LISA to Antarctica for the first time ever, to analyse shallow snow and firn cores directly in the field.

    This is part of our contribution to the EPIC iQ2300 – a project led by Prof. Arjen Stroeven in Stockholm and organised by the Swedish Polar Research Secretariat.

    iQ2300 is a huge project, and we are just a small part of it: the aim is to understand Dronning Maud Land’s evolution from the Holocene and out to 2300. Expect to hear a lot more about this effort in coming months…

    Map of Antarctica, I lifted from polar.se : LISA will be visiting the Swedish Wasa station in DML – the top bit on this map – with us

    Now back to our humble friend.

    We hope LISA will help us understand how much snow falls in Dronning Maud Land, how much it varies from year to year and what is the influence of sea ice and far field atmospheric processes on the rate of snowfall. Snowfall is exceptionally difficult to measure and one of our biggest uncertainties in working out Antarctic mass budget and the response of Antarctica to a changing climate (spoiler alert: we might have a paper coming out about this shortly)…

    Meet LISA: a view inside the Magic Box..

    Although LISA has been used in Greenland before, this is quite an experimental deployment, which means potentially really a lot of valuable scientific results. We would ultimately liek to build an Antarctic specific box, but that will have to wait to see if the results of this deployment are as good as we hope. (And some funding – if you are a billionaire with a spare couple of hundred thousand Euros, we’re always interested in talking).

    The box itself is conceptually simple but in practice a little complex with a multiplicity of tubes, connectors and spare parts. This means it’s easy to fix if it breaks down, but also we need to understand how it works first.

    Some parts of LISA are quite fiddly…

    Today, the awesome and exceptionally generous Associate Professor Helle Kjær took myself, Stockholm Uni Prof Ninis Rosqvist and our PhD colleague from the Novo Nordisk funded PRECISE project, Clément Cherblanc through the use of the box.

    Helle showing Clément the workings inside LISA

    There’s a lot to remember and a lot to check but we’re reasonably hopeful we’ll get good results. The aim is to understand both the interannual variability on decadal timescales and the spatial gradients in snowfall accumulation. It’s a huge task, so it’s probably fortunate that we have 6 weeks or so (depending on the weather always!) to try and get it deployed at anumber of different sites which will hopefully allow us to do this.

    It’s a big change to my normal fieldwork activities, but also a logical extension of them. And highly complementary to the climate and SMB modelling we are developing.

    Nonetheless, ithere’s a lot of new stuff and I have in the past weeks learnt a great deal about transporting very small amounts of mildly hazardous chemicals on airlines, how to deal with customs and pack fragile instruments in large boxes.

    Much more to come on this project, so stay tuned…

    Clement getting stuck into using the software that measures different properties in the cores.

    #PolarSekretariatet #AntarcticFieldwork #IceClimate #PolarClimate #Snow #SMB #AtmosphericVariability #iceCores #FirnCores #SnowCores

    #Antarctica #AntarcticFieldwork #AtmosphericVariability #climateChange #firn #FirnCores #IceClimate #iceCores #iQ2300 #PolarClimate #PolarSekretariatet #smb #snow #SnowCores

  3. Meeting LISA

    LISA: the Lightweight In Situ Analysis box is one of a kind; built by our friends at PICE in the Niels Bohr Institute. Later this year we’re taking LISA to Antarctica for the first time ever, to analyse shallow snow and firn cores directly in the field.

    This is part of our contribution to the EPIC iQ2300 – a project led by Prof. Arjen Stroeven in Stockholm and organised by the Swedish Polar Research Secretariat.

    iQ2300 is a huge project, and we are just a small part of it: the aim is to understand Dronning Maud Land’s evolution from the Holocene and out to 2300. Expect to hear a lot more about this effort in coming months…

    Map of Antarctica, I lifted from polar.se : LISA will be visiting the Swedish Wasa station in DML – the top bit on this map – with us

    Now back to our humble friend.

    We hope LISA will help us understand how much snow falls in Dronning Maud Land, how much it varies from year to year and what is the influence of sea ice and far field atmospheric processes on the rate of snowfall. Snowfall is exceptionally difficult to measure and one of our biggest uncertainties in working out Antarctic mass budget and the response of Antarctica to a changing climate (spoiler alert: we might have a paper coming out about this shortly)…

    Meet LISA: a view inside the Magic Box..

    Although LISA has been used in Greenland before, this is quite an experimental deployment, which means potentially really a lot of valuable scientific results. We would ultimately liek to build an Antarctic specific box, but that will have to wait to see if the results of this deployment are as good as we hope. (And some funding – if you are a billionaire with a spare couple of hundred thousand Euros, we’re always interested in talking).

    The box itself is conceptually simple but in practice a little complex with a multiplicity of tubes, connectors and spare parts. This means it’s easy to fix if it breaks down, but also we need to understand how it works first.

    Some parts of LISA are quite fiddly…

    Today, the awesome and exceptionally generous Associate Professor Helle Kjær took myself, Stockholm Uni Prof Ninis Rosqvist and our PhD colleague from the Novo Nordisk funded PRECISE project, Clément Cherblanc through the use of the box.

    Helle showing Clément the workings inside LISA

    There’s a lot to remember and a lot to check but we’re reasonably hopeful we’ll get good results. The aim is to understand both the interannual variability on decadal timescales and the spatial gradients in snowfall accumulation. It’s a huge task, so it’s probably fortunate that we have 6 weeks or so (depending on the weather always!) to try and get it deployed at anumber of different sites which will hopefully allow us to do this.

    It’s a big change to my normal fieldwork activities, but also a logical extension of them. And highly complementary to the climate and SMB modelling we are developing.

    Nonetheless, ithere’s a lot of new stuff and I have in the past weeks learnt a great deal about transporting very small amounts of mildly hazardous chemicals on airlines, how to deal with customs and pack fragile instruments in large boxes.

    Much more to come on this project, so stay tuned…

    Clement getting stuck into using the software that measures different properties in the cores.

    #PolarSekretariatet #AntarcticFieldwork #IceClimate #PolarClimate #Snow #SMB #AtmosphericVariability #iceCores #FirnCores #SnowCores

    #Antarctica #AntarcticFieldwork #AtmosphericVariability #climateChange #firn #FirnCores #IceClimate #iceCores #iQ2300 #PolarClimate #PolarSekretariatet #smb #snow #SnowCores

  4. Meeting LISA

    LISA: the Lightweight In Situ Analysis box is one of a kind; built by our friends at PICE in the Niels Bohr Institute. Later this year we’re taking LISA to Antarctica for the first time ever, to analyse shallow snow and firn cores directly in the field.

    This is part of our contribution to the EPIC iQ2300 – a project led by Prof. Arjen Stroeven in Stockholm and organised by the Swedish Polar Research Secretariat.

    iQ2300 is a huge project, and we are just a small part of it: the aim is to understand Dronning Maud Land’s evolution from the Holocene and out to 2300. Expect to hear a lot more about this effort in coming months…

    Map of Antarctica, I lifted from polar.se : LISA will be visiting the Swedish Wasa station in DML – the top bit on this map – with us

    Now back to our humble friend.

    We hope LISA will help us understand how much snow falls in Dronning Maud Land, how much it varies from year to year and what is the influence of sea ice and far field atmospheric processes on the rate of snowfall. Snowfall is exceptionally difficult to measure and one of our biggest uncertainties in working out Antarctic mass budget and the response of Antarctica to a changing climate (spoiler alert: we might have a paper coming out about this shortly)…

    Meet LISA: a view inside the Magic Box..

    Although LISA has been used in Greenland before, this is quite an experimental deployment, which means potentially really a lot of valuable scientific results. We would ultimately liek to build an Antarctic specific box, but that will have to wait to see if the results of this deployment are as good as we hope. (And some funding – if you are a billionaire with a spare couple of hundred thousand Euros, we’re always interested in talking).

    The box itself is conceptually simple but in practice a little complex with a multiplicity of tubes, connectors and spare parts. This means it’s easy to fix if it breaks down, but also we need to understand how it works first.

    Some parts of LISA are quite fiddly…

    Today, the awesome and exceptionally generous Associate Professor Helle Kjær took myself, Stockholm Uni Prof Ninis Rosqvist and our PhD colleague from the Novo Nordisk funded PRECISE project, Clément Cherblanc through the use of the box.

    Helle showing Clément the workings inside LISA

    There’s a lot to remember and a lot to check but we’re reasonably hopeful we’ll get good results. The aim is to understand both the interannual variability on decadal timescales and the spatial gradients in snowfall accumulation. It’s a huge task, so it’s probably fortunate that we have 6 weeks or so (depending on the weather always!) to try and get it deployed at anumber of different sites which will hopefully allow us to do this.

    It’s a big change to my normal fieldwork activities, but also a logical extension of them. And highly complementary to the climate and SMB modelling we are developing.

    Nonetheless, ithere’s a lot of new stuff and I have in the past weeks learnt a great deal about transporting very small amounts of mildly hazardous chemicals on airlines, how to deal with customs and pack fragile instruments in large boxes.

    Much more to come on this project, so stay tuned…

    Clement getting stuck into using the software that measures different properties in the cores.

    #PolarSekretariatet #AntarcticFieldwork #IceClimate #PolarClimate #Snow #SMB #AtmosphericVariability #iceCores #FirnCores #SnowCores

    #Antarctica #AntarcticFieldwork #AtmosphericVariability #climateChange #firn #FirnCores #IceClimate #iceCores #iQ2300 #PolarClimate #PolarSekretariatet #smb #snow #SnowCores

  5. Meeting LISA

    LISA: the Lightweight In Situ Analysis box is one of a kind; built by our friends at PICE in the Niels Bohr Institute. Later this year we’re taking LISA to Antarctica for the first time ever, to analyse shallow snow and firn cores directly in the field.

    This is part of our contribution to the EPIC iQ2300 – a project led by Prof. Arjen Stroeven in Stockholm and organised by the Swedish Polar Research Secretariat.

    iQ2300 is a huge project, and we are just a small part of it: the aim is to understand Dronning Maud Land’s evolution from the Holocene and out to 2300. Expect to hear a lot more about this effort in coming months…

    Map of Antarctica, I lifted from polar.se : LISA will be visiting the Swedish Wasa station in DML – the top bit on this map – with us

    Now back to our humble friend.

    We hope LISA will help us understand how much snow falls in Dronning Maud Land, how much it varies from year to year and what is the influence of sea ice and far field atmospheric processes on the rate of snowfall. Snowfall is exceptionally difficult to measure and one of our biggest uncertainties in working out Antarctic mass budget and the response of Antarctica to a changing climate (spoiler alert: we might have a paper coming out about this shortly)…

    Meet LISA: a view inside the Magic Box..

    Although LISA has been used in Greenland before, this is quite an experimental deployment, which means potentially really a lot of valuable scientific results. We would ultimately liek to build an Antarctic specific box, but that will have to wait to see if the results of this deployment are as good as we hope. (And some funding – if you are a billionaire with a spare couple of hundred thousand Euros, we’re always interested in talking).

    The box itself is conceptually simple but in practice a little complex with a multiplicity of tubes, connectors and spare parts. This means it’s easy to fix if it breaks down, but also we need to understand how it works first.

    Some parts of LISA are quite fiddly…

    Today, the awesome and exceptionally generous Associate Professor Helle Kjær took myself, Stockholm Uni Prof Ninis Rosqvist and our PhD colleague from the Novo Nordisk funded PRECISE project, Clément Cherblanc through the use of the box.

    Helle showing Clément the workings inside LISA

    There’s a lot to remember and a lot to check but we’re reasonably hopeful we’ll get good results. The aim is to understand both the interannual variability on decadal timescales and the spatial gradients in snowfall accumulation. It’s a huge task, so it’s probably fortunate that we have 6 weeks or so (depending on the weather always!) to try and get it deployed at anumber of different sites which will hopefully allow us to do this.

    It’s a big change to my normal fieldwork activities, but also a logical extension of them. And highly complementary to the climate and SMB modelling we are developing.

    Nonetheless, ithere’s a lot of new stuff and I have in the past weeks learnt a great deal about transporting very small amounts of mildly hazardous chemicals on airlines, how to deal with customs and pack fragile instruments in large boxes.

    Much more to come on this project, so stay tuned…

    Clement getting stuck into using the software that measures different properties in the cores.

    #PolarSekretariatet #AntarcticFieldwork #IceClimate #PolarClimate #Snow #SMB #AtmosphericVariability #iceCores #FirnCores #SnowCores

    #Antarctica #AntarcticFieldwork #AtmosphericVariability #climateChange #firn #FirnCores #IceClimate #iceCores #iQ2300 #PolarClimate #PolarSekretariatet #smb #snow #SnowCores

  6. Meeting LISA

    LISA: the Lightweight In Situ Analysis box is one of a kind; built by our friends at PICE in the Niels Bohr Institute. Later this year we’re taking LISA to Antarctica for the first time ever, to analyse shallow snow and firn cores directly in the field.

    This is part of our contribution to the EPIC iQ2300 – a project led by Prof. Arjen Stroeven in Stockholm and organised by the Swedish Polar Research Secretariat.

    iQ2300 is a huge project, and we are just a small part of it: the aim is to understand Dronning Maud Land’s evolution from the Holocene and out to 2300. Expect to hear a lot more about this effort in coming months…

    Map of Antarctica, I lifted from polar.se : LISA will be visiting the Swedish Wasa station in DML – the top bit on this map – with us

    Now back to our humble friend.

    We hope LISA will help us understand how much snow falls in Dronning Maud Land, how much it varies from year to year and what is the influence of sea ice and far field atmospheric processes on the rate of snowfall. Snowfall is exceptionally difficult to measure and one of our biggest uncertainties in working out Antarctic mass budget and the response of Antarctica to a changing climate (spoiler alert: we might have a paper coming out about this shortly)…

    Meet LISA: a view inside the Magic Box..

    Although LISA has been used in Greenland before, this is quite an experimental deployment, which means potentially really a lot of valuable scientific results. We would ultimately liek to build an Antarctic specific box, but that will have to wait to see if the results of this deployment are as good as we hope. (And some funding – if you are a billionaire with a spare couple of hundred thousand Euros, we’re always interested in talking).

    The box itself is conceptually simple but in practice a little complex with a multiplicity of tubes, connectors and spare parts. This means it’s easy to fix if it breaks down, but also we need to understand how it works first.

    Some parts of LISA are quite fiddly…

    Today, the awesome and exceptionally generous Associate Professor Helle Kjær took myself, Stockholm Uni Prof Ninis Rosqvist and our PhD colleague from the Novo Nordisk funded PRECISE project, Clément Cherblanc through the use of the box.

    Helle showing Clément the workings inside LISA

    There’s a lot to remember and a lot to check but we’re reasonably hopeful we’ll get good results. The aim is to understand both the interannual variability on decadal timescales and the spatial gradients in snowfall accumulation. It’s a huge task, so it’s probably fortunate that we have 6 weeks or so (depending on the weather always!) to try and get it deployed at anumber of different sites which will hopefully allow us to do this.

    It’s a big change to my normal fieldwork activities, but also a logical extension of them. And highly complementary to the climate and SMB modelling we are developing.

    Nonetheless, ithere’s a lot of new stuff and I have in the past weeks learnt a great deal about transporting very small amounts of mildly hazardous chemicals on airlines, how to deal with customs and pack fragile instruments in large boxes.

    Much more to come on this project, so stay tuned…

    Clement getting stuck into using the software that measures different properties in the cores.

    #PolarSekretariatet #AntarcticFieldwork #IceClimate #PolarClimate #Snow #SMB #AtmosphericVariability #iceCores #FirnCores #SnowCores

    #Antarctica #AntarcticFieldwork #AtmosphericVariability #climateChange #firn #FirnCores #IceClimate #iceCores #iQ2300 #PolarClimate #PolarSekretariatet #smb #snow #SnowCores

  7. From my Front Door R8I4

    Nature’s Cycle: Life from Death

    1/25, f/8, tripod, shutter release cable
    Film (R9): Ilford XP2 Super 400, ISO400,
    Camera: Zeiss Ikon Ikonta 521/2, Zeiss Tessar 4.5 / 10.5cm
    Film developed by TheDarkRoom, San Clemente, CA
    Super Scan

    #photography #photo #beliefeinfilm #blackandwhitephotography #blackandwhite #firn #intothewoods #moody #zeissikonikonta #filmisnotdead #ilfordxp2super400

    flic.kr/p/2qoxZ62

  8. From my Front Door R8I4

    Nature’s Cycle: Life from Death

    1/25, f/8, tripod, shutter release cable
    Film (R9): Ilford XP2 Super 400, ISO400,
    Camera: Zeiss Ikon Ikonta 521/2, Zeiss Tessar 4.5 / 10.5cm
    Film developed by TheDarkRoom, San Clemente, CA
    Super Scan

    #photography #photo #beliefeinfilm #blackandwhitephotography #blackandwhite #firn #intothewoods #moody #zeissikonikonta #filmisnotdead #ilfordxp2super400

    flic.kr/p/2qoxZ62

  9. From my Front Door R8I4

    Nature’s Cycle: Life from Death

    1/25, f/8, tripod, shutter release cable
    Film (R9): Ilford XP2 Super 400, ISO400,
    Camera: Zeiss Ikon Ikonta 521/2, Zeiss Tessar 4.5 / 10.5cm
    Film developed by TheDarkRoom, San Clemente, CA
    Super Scan

    #photography #photo #beliefeinfilm #blackandwhitephotography #blackandwhite #firn #intothewoods #moody #zeissikonikonta #filmisnotdead #ilfordxp2super400

    flic.kr/p/2qoxZ62

  10. From my Front Door R8I4

    Nature’s Cycle: Life from Death

    1/25, f/8, tripod, shutter release cable
    Film (R9): Ilford XP2 Super 400, ISO400,
    Camera: Zeiss Ikon Ikonta 521/2, Zeiss Tessar 4.5 / 10.5cm
    Film developed by TheDarkRoom, San Clemente, CA
    Super Scan

    #photography #photo #beliefeinfilm #blackandwhitephotography #blackandwhite #firn #intothewoods #moody #zeissikonikonta #filmisnotdead #ilfordxp2super400

    flic.kr/p/2qoxZ62

  11. From my Front Door R8I4

    Nature’s Cycle: Life from Death

    1/25, f/8, tripod, shutter release cable
    Film (R9): Ilford XP2 Super 400, ISO400,
    Camera: Zeiss Ikon Ikonta 521/2, Zeiss Tessar 4.5 / 10.5cm
    Film developed by TheDarkRoom, San Clemente, CA
    Super Scan

    #photography #photo #beliefeinfilm #blackandwhitephotography #blackandwhite #firn #intothewoods #moody #zeissikonikonta #filmisnotdead #ilfordxp2super400

    flic.kr/p/2qoxZ62

  12. Waiting for the handyman.
    Reading a paper on analyzing firn in Antarctica. Firn is the snow layer before it gets compacted to actual ice. The firn layer contains gas like methane or CO2, too, but the air bubbles aren't strictly sorted on input date 😁 The bubbles can be older or younger than their immediate surrounding. (True for real ice layers, too.)

    All very interesting.
    tc.copernicus.org/articles/13/
    "Multi-tracer study of gas trapping in an East Antarctic ice core" by Kevin #Fourteau et al 2019.

    The absolute shocking byproduct of their incredibly thorough work is a 2700 year data series for CH4 in MONTHLY resolution!! doi.pangaea.de/10.1594/PANGAEA

    From -930 to 1774 AD.
    Their gas dating method is so exact that they pinpoint several different days for every month, too.

    I am stunned that monthly resolution is possible. And this was merely a byproduct of figuring out the best way to analyze firn.

    #paleoclimate #methane #CH4 #firn #icecore #ice #snow #Antarctica

  13. Greenland firn analysis with NIR-HSI reveals ice sheet meltwater dynamics.

    "A Cold Laboratory Hyperspectral Imaging System Mapping #Firn Core #Grain Size and #Ice Layer #Stratigraphy" at #AGU23 includes collaboration with Critical Zone Network Dust^2 members.

    🔗🗓️ bit.ly/agu23121405

  14. Looking forward to the #FIRN community of academics visiting nipaluna #hobart for the 2023 Financial Research Network Annual Conference and #PhD symposium in November. Welcome to lutruwita #tasmania and to the University of Tasmania! Impressive line up of papers lnkd.in/g6ugxcSD Thank you Elvira, Marco, Nelson & the organisation and review committees for creating this great event #university #finance #ESG #volatility #trading #behaviour #regulation #bonds #funds #realestate #liquidity #innovation #institutions

  15. The #Antarctic Ice Sheet is covered by a thick layer of #firn, snow that is compressed to ice. At present it protects vulnerable parts from the impact of surface melt, but what will this look like in the future? Our preprint paper is out now, spearheaded by my colleague @sanneveldhuijsen ! egusphere.copernicus.org/prepr

  16. INterested in #Firn + #snow in #Antarctica? Just read this paper by Brooke Medley and it's a really nice piece of work..

    tc.copernicus.org/articles/16/