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Record W2319686951 · doi:10.3354/cr00996

Vanishing winters in Germany: soil frost dynamics and snow cover trends, and ecological implications

2011· article· en· W2319686951 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.

Bibliographic record

VenueClimate Research · 2011
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicClimate change and permafrost
Canadian institutionsWestern University
Fundersnot available
KeywordsSnow coverSnowFrost (temperature)Temperate climatePhysical geographyEcologyGeographyEnvironmental scienceClimate changeClimatologyMeteorologyBiologyGeology

Abstract

fetched live from OpenAlex

CR Climate Research Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsSpecials CR 46:269-276 (2011) - DOI: https://doi.org/10.3354/cr00996 Vanishing winters in Germany: soil frost dynamics and snow cover trends, and ecological implications Juergen Kreyling1,*, Hugh A. L. Henry2 1University of Bayreuth, Biogeography, 95440 Bayreuth, Germany 2University of Western Ontario, Biology, London, Ontario N6A 5B7, Canada *Email: juergen.kreyling@uni-bayreuth.de ABSTRACT: Current climate models are effective at projecting trends in mean winter temperature; however, other ecologically relevant parameters—such as snow cover and soil frost dynamics—are less well investigated. Changes in these parameters are expected to have strong ecological implications, especially in the temperate zone, where it is uncertain whether snow and soil frost will occur with regularity in the future. We explored trends in days with snow on the ground (snowdays), minimum soil temperature (MST), and number of soil freeze/thaw cycles (FTCs, i.e. changes in sign from negative to positive in any pair of consecutive soil temperature records at 5 cm depth) at 177 German weather stations for 1950–2000. Future trends were explored by statistical modelling based on climatic and topographic predictors. Snowdays decreased uniformly at a rate of 0.5 d yr–1 in the recent past. This trend is projected to continue to a point where significant parts of Germany will no longer regularly experience snow cover. MST has increased, and is projected to do so in the future, mainly in southern Germany. FTCs have been decreasing uniformly in the recent past. No evidence for increased FTCs or decreased MST with decreasing insulation due to missing snow cover was found. FTCs are projected to decrease disproportionately in northeastern Germany, where past frequencies were higher. Ecological implications of the significant decrease in the occurrence and magnitude of the climate parameters studied include changes in nutrient cycling, productivity and survival of organisms over­wintering at the soil surface. Ecological research is needed, as the effects of diminished winters on ecosystems are not well understood. KEY WORDS: Winter climate change · Winter ecology · Freezing-thawing · Soil freezing · ­Temperate systems Full text in pdf format PreviousNextCite this article as: Kreyling J, Henry HAL (2011) Vanishing winters in Germany: soil frost dynamics and snow cover trends, and ecological implications. Clim Res 46:269-276. https://doi.org/10.3354/cr00996 Export citation RSS - Facebook - Tweet - linkedIn Cited by Published in CR Vol. 46, No. 3. Online publication date: May 19, 2011 Print ISSN: 0936-577X; Online ISSN: 1616-1572 Copyright © 2011 Inter-Research.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.085
Threshold uncertainty score0.995

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0060.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.146
GPT teacher head0.341
Teacher spread0.195 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it