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17 (0,127s) •

Project

Distribution, Thickness and Evolution of Permafrost in Central Europe in Late Quaternary (GA21-23196S)

permafrost changes in non-alpine Central Europe. We intend to answer still-discussed and largely unresolved problems of what were the glacier–permafrost interactions around the southern limit of the Scandinavian ice sheet, how ...

Geology

  • 2021 - 2023
    • •
  • 6 268 tis. Kč
    • •
  • 6 268 tis. Kč
    • •
  • GA ČR
Project

Dynamics of the periglacial environment in the Antarctic Peninsula region under ongoing climate change (GM22-28659M)

The active layer and permafrost are the building elements of the periglacial environment in polar regions. Their parameters like temperature, moisture, or active layer and permafrost temperature belongs to principal questions of An...

Climatic research

  • 2022 - 2026
    • •
  • 19 287 tis. Kč
    • •
  • 19 287 tis. Kč
    • •
  • GA ČR
Project

Soil Moisture Effects on Active Layer and Permafrost Dynamics in the Antarctic Peninsula (LL2505)

alterations in their functioning, including impacts on the soil environment and permafrost of the active layer and permafrost. The specific objectives of the project focus on: 1 in the thickness of the active layer, temperature at ...

Physical geography

  • 2025 - 2027
    • •
  • 14 786 tis. Kč
    • •
  • 14 786 tis. Kč
    • •
  • MŠMT
Project

Determining the influence of frost heave and thaw settlement on the thermal regime of frozen ground and its implementation in freeze-thaw models (GA25-18272S)

Vertical ground deformations due to frost heave and thaw settlement are important features in regions of permafrost and seasonally frozen ground, often causing physical modelling experiments simulating permafrost and seasonally froz...

Physical geography

  • 2025 - 2027
    • •
  • 7 200 tis. Kč
    • •
  • 7 200 tis. Kč
    • •
  • GA ČR
Project

Microbiomes of Selected Extreme Biotopes – Their Phylogenetic Diversity and Functional Potential (LTAUSA19028)

The objective of the proposed project is to characterize microbial populations in extreme biotopes – chronosequence of permafrost (permafrost of differing age) from central Alaska and soils from salt marshes and moffettes of the Soo...

Ecology

  • 2019 - 2022
    • •
  • 6 177 tis. Kč
    • •
  • 6 177 tis. Kč
    • •
  • MŠMT
Project

Cryogenic cave carbonates Mechanisms of formation and relationship to permafrost depth (GAP210/10/1760)

, minimum permafrost depth during the Last Glacial Maximum will be estimated...

DB - Geologie a mineralogie

  • 2010 - 2012
    • •
  • 1 327 tis. Kč
    • •
  • 1 327 tis. Kč
    • •
  • GA ČR
Project

CRYOVULCAN - Vulnerability of carbon in Cryosols – substrate-microorganisms-aggregate interactions (GC20-21259J)

Thawing of the permafrost may result in two contrasting scenarios of the active layer: wetter or drier soil. The main objective of the project is to comparatively investigate OM decomposition and stabilization under these two scenarios. Our ...

Climatic research

  • 2020 - 2023
    • •
  • 9 131 tis. Kč
    • •
  • 9 131 tis. Kč
    • •
  • GA ČR
Project

Multiphase flow, transport, and structural changes related to water freezing and thawing in the subsurface (GA21-09093S)

The on-going climate changes observed during last decades cause release of methane and other gases from thawing permafrost in arctic regions. Understanding the fundamental processes of freezing or thawing of a porous medium containing fluid,...

Applied mathematics

  • 2021 - 2023
    • •
  • 7 766 tis. Kč
    • •
  • 7 766 tis. Kč
    • •
  • GA ČR
Project

Significance of ice-retaining screes as natural landscape global climate change observation system (GA205/06/1236)

voids, (ii) to document existence of azonal permafrost in ice-retaining screes, (iii...

DG - Vědy o atmosféře, meteorologie

  • 2006 - 2008
    • •
  • 971 tis. Kč
    • •
  • 971 tis. Kč
    • •
  • GA ČR
Project

Long-term Carbon Storage in Cryoturbeated Arctic Soils (7E10073)

The total organic carbon pool of soils (SOC) of the circum-arctic permafrost zone has been estimated to contain ~400 Gt C in the upper 1m and as much as 747 Gt C in the upper 3m, excluding peatlands and carbon in deep loess sediment reservoi...

DF - Pedologie

  • 2010 - 2013
    • •
  • 4 301 tis. Kč
    • •
  • 4 301 tis. Kč
    • •
  • MŠMT
  • 1 - 10 out of 17