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Journal articles on the topic 'Chaîne de compilation'

Author: Grafiati

Published: 8 June 2024

Last updated: 31 July 2025

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1

Bennas, Nard, and Carmen Elisa Sàinz-Cantero. "Coléoptères aquatiques Adephaga de la chaîne rifaine marocaine (Coleoptera Gyrinidae, Haliplidae, Noteridae, Hygrobiidae, Dytiscidae)." Memorie della Società Entomologica Italiana 85, no. 1 (2006): 31. http://dx.doi.org/10.4081/memoriesei.2006.31.

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Une étude sur 4041 individus adultes de Coléoptères aquatiques Adephaga récoltés dans diverses localités de la chaîne rifaine marocaine a permis l’identification de 61 espèces dont une (<em>Hydroporus memnonius</em>) s’avère nouvelle pour le Maroc et 6 pour le territoire rifain. Les données obtenues lors des prospections et la compilation des citations bibliographiques concernant ce groupe d’insectes, ont permis la réalisation de l’inventaire des 81 espèces connues jusqu’à présent pour les neuf provinces faisant partie du Rif.

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Mas, Élodie. "Las evidencias de producción en material malacológico: análisis tecnológico de las colecciones de Sayula (Jalisco)." Revista Trace, no. 76 (July 31, 2019): 167. http://dx.doi.org/10.22134/trace.76.2019.129.

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Durante el periodo comprendido entre 450 y 1000 d.C., las conchas marinas desempeñan un papel fundamental en las dinámicas socioeconómicas y culturales de las poblaciones asentadas en la región de la cuenca de Sayula. El material malacológico asociado a este periodo ofrece datos inéditos por contar con numerosas evidencias de producción que reflejan una manufactura local de ornamentos de concha. Esta investigación se presenta como una guía metodológica, enfocada al análisis de huellas técnicas, que permite clasificar cada pieza según su grado de transformación y determinar su lugar en la caden

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Jovanovic, S., and S. Weber. "Modélisation SystemC-TLM de systèmes à base de processeur." J3eA 18 (2019): 1009. http://dx.doi.org/10.1051/j3ea/20191009.

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Nous présentons un ensemble de travaux pratiques qui seront dispensés au sein du Master EEA - Électronique Embarquée à l'université de Lorraine dans le cadre du module « Modélisation SystemC ». Ces TP sont destinés à initier les étudiants à la modélisation de systèmes et circuits numériques en SystemC-TLM et sont organisés autour de la suite logicielle open source Eclipse et de la chaine de compilation gcc pour la simulation, test et vérification.

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Prado, L. F., I. Wainer, C. M. Chiessi, M. P. Ledru, and B. Turcq. "Mid-Holocene climate reconstruction for eastern South America." Climate of the Past Discussions 8, no. 6 (2012): 5925–61. http://dx.doi.org/10.5194/cpd-8-5925-2012.

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Abstract. The Mid-Holocene (6 ka BP) is a key period to the study of climate, since it presented lower than present incoming summer insolation in the Southern Hemisphere, and the opposite in the Northern Hemisphere. This happened due to a different than present configuration of the orbital parameters. To investigate the effects of insolation on the Mid-Holocene climate, some global and regional multiproxy palaeodata compilations have been elaborated. However, few global studies have focused on the Southern Hemisphere, and none of the regional ones have characterized the Mid-Holocene climate in

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Suhaciov, Nikolaj, and Svetlana Kokoškina. "La géographie linguistique en Union soviétique : les atlas linguistiques." Cahiers du Centre de Linguistique et des Sciences du Langage, no. 40 (October 12, 2014): 131–54. http://dx.doi.org/10.26034/la.cdclsl.2014.677.

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Cet article aborde l’évolution de la recherche dialectologique en Union soviétique dès les origines jusqu’aux années 1980. Il suit en détail les principes et les méthodes de compilation des atlas linguistiques sur le matériau des langues slaves. Deux écoles de géographie linguistique, leningradoise et moscovite, ont coexisté et développé chacune une approche originale du matériau linguistique. Les auteurs cherchent à décrypter les principes linguistiques adoptés, les visées des auteurs des atlas, et, surtout, les zones décrites.

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Peterson, Carlye D., та Lorraine E. Lisiecki. "Deglacial carbon cycle changes observed in a compilation of 127 benthic <i>δ</i><sup>13</sup>C time series (20–6 ka)". Climate of the Past 14, № 8 (2018): 1229–52. http://dx.doi.org/10.5194/cp-14-1229-2018.

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Abstract. We present a compilation of 127 time series δ13C records from Cibicides wuellerstorfi spanning the last deglaciation (20–6 ka) which is well-suited for reconstructing large-scale carbon cycle changes, especially for comparison with isotope-enabled carbon cycle models. The age models for the δ13C records are derived from regional planktic radiocarbon compilations (Stern and Lisiecki, 2014). The δ13C records were stacked in nine different regions and then combined using volume-weighted averages to create intermediate, deep, and global δ13C stacks. These benthic δ13C stacks are used to

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Christiansen, B., and F. C. Ljungqvist. "The extra-tropical Northern Hemisphere temperature in the last two millennia: reconstructions of low-frequency variability." Climate of the Past 8, no. 2 (2012): 765–86. http://dx.doi.org/10.5194/cp-8-765-2012.

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Abstract. We present two new multi-proxy reconstructions of the extra-tropical Northern Hemisphere (30–90° N) mean temperature: a two-millennia long reconstruction reaching back to 1 AD and a 500-yr long reconstruction reaching back to 1500 AD. The reconstructions are based on compilations of 32 and 91 proxies, respectively, of which only little more than half pass a screening procedure and are included in the actual reconstructions. The proxies are of different types and of different resolutions (annual, annual-to-decadal, and decadal) but all have previously been shown to relate to local or

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Albani, S., N. M. Mahowald, G. Winckler, et al. "Twelve thousand years of dust: the Holocene global dust cycle constrained by natural archives." Climate of the Past Discussions 10, no. 6 (2014): 4277–363. http://dx.doi.org/10.5194/cpd-10-4277-2014.

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Abstract. Mineral dust plays an important role in the climate system by interacting with radiation, clouds, and biogeochemical cycles. In addition, natural archives show that the dust cycle experienced variability in the past in response to global and local climate change. The compilation of the DIRTMAP paleodust datasets in the last two decades provided a target for paleoclimate models that include the dust cycle, following a time slice approach. We propose an innovative framework to organize a paleodust dataset that moves on from the positive experience of DIRTMAP and takes into account new

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Albani, S., N. M. Mahowald, G. Winckler, et al. "Twelve thousand years of dust: the Holocene global dust cycle constrained by natural archives." Climate of the Past 11, no. 6 (2015): 869–903. http://dx.doi.org/10.5194/cp-11-869-2015.

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Abstract. Mineral dust plays an important role in the climate system by interacting with radiation, clouds, and biogeochemical cycles. In addition, natural archives show that the dust cycle experienced variability in the past in response to global and local climate change. The compilation of the DIRTMAP (Dust Indicators and Records from Terrestrial and MArine Palaeoenvironments) paleodust data sets in the last 2 decades provided a benchmark for paleoclimate models that include the dust cycle, following a time slice approach. We propose an innovative framework to organize a paleodust data set t

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Nieto Masot, Ana, and José Luis Gurría Gascón. "Sustainable Rural Development: Strategies, Good Practices and Opportunities (Second Edition)." Land 13, no. 1 (2024): 104. http://dx.doi.org/10.3390/land13010104.

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In 2021, a book entitled “Sustainable Rural Development: Strategies, Good Practices and Opportunities” was launched as a compilation of 16 papers and published in a Special Issue of the journal Land [...]

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Chastang, Pierre, Laurent Feller, and Jean-Marie Martin. "Autour de l’édition du Registrum Petri Diaconi. Problèmes de documentation cassinésienne : chartes, rouleaux, registre." Mélanges de l École française de Rome Moyen Âge 121, no. 1 (2009): 99–135. http://dx.doi.org/10.3406/mefr.2009.9487.

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Le Registrum Petri Diaconi, cartulaire général du Mont-Cassin compilé entre 1131 et 1133, dont on prépare l’édition, a déjà été mis en rapports avec les Chronica monasterii Casinensis. Il est, en outre, le seul des grands cartulaires compilés à cette époque dans l’Italie centro-méridionale que l’on peut confronter aux archives de l’abbaye, dont l’essentiel a été préservé. Environ 160 des 716 documents qu’il contient sont encore conservés en originaux, d’autres sous la forme de copies anciennes, dont certaines se trouvent dans des registres et autres manuscrits de l’abbaye, qui possède égalemen

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Chadwick, Matthew, Xavier Crosta, Oliver Esper, Lena Thöle, and Karen E. Kohfeld. "Compilation of Southern Ocean sea-ice records covering the last glacial-interglacial cycle (12–130 ka)." Climate of the Past 18, no. 8 (2022): 1815–29. http://dx.doi.org/10.5194/cp-18-1815-2022.

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Abstract. Antarctic sea ice forms a critical part of the Southern Ocean and global climate system. The behaviour of Antarctic sea ice throughout the last glacial-interglacial (G-IG) cycle (12 000–130 000 years) allows us to investigate the interactions between sea ice and climate under a large range of mean climate states. Understanding both temporal and spatial variations in Antarctic sea ice across a G-IG cycle is crucial to a better understanding of the G-IG regulation of atmospheric CO2, ocean circulation, nutrient cycling and productivity. This study presents 28 published qualitative and

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Lang, N., and E. W. Wolff. "Interglacial and glacial variability from the last 800 ka in marine, ice and terrestrial archives." Climate of the Past 7, no. 2 (2011): 361–80. http://dx.doi.org/10.5194/cp-7-361-2011.

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Abstract. We have compiled 37 ice, marine and terrestrial palaeoclimate records covering the last 800 000 years in order to assess the pattern of glacial and interglacial strength, and termination amplitude. Records were selected based on their length, completeness and resolution, and their age models were updated, where required, by alignment to the LR04 benthic δ18O stack. The resulting compilation allows comparison of individual glacial to interglacial transitions with confidence, but the level of synchronisation is inadequate for discussion of temporal phasing. The comparison of interglaci

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Lang, N., and E. W. Wolff. "Interglacial and glacial variability from the last 800 ka in marine, ice and terrestrial archives." Climate of the Past Discussions 6, no. 5 (2010): 2223–66. http://dx.doi.org/10.5194/cpd-6-2223-2010.

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Abstract. We have compiled 37 ice, marine and terrestrial palaeoclimate records covering the last 800 000 years in order to assess the pattern of glacial and interglacial strength, and termination amplitude. Records were selected based on their length, completeness and resolution, and their age models were updated, where required, by alignment to the LR04 benthic δ18O stack. The resulting compilation allows comparison of individual glacial to interglacial transitions with confidence, but the level of synchronisation is inadequate for discussion of temporal phasing. The comparison of interglaci

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15

Mairesse, A., H. Goosse, P. Mathiot, H. Wanner, and S. Dubinkina. "Investigating the consistency between proxies and between proxies and models using data assimilation: a mid-Holocene case study." Climate of the Past Discussions 9, no. 4 (2013): 3953–91. http://dx.doi.org/10.5194/cpd-9-3953-2013.

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Abstract. The mid-Holocene (6 thousand years before present) is a key period to study the consistency between model results and proxy data as it corresponds to a standard test for models and a reasonable number of proxy records are available. Taking advantage of this relatively large amount of information, we have first compared a compilation of 50 air and sea surface temperature reconstructions with the results of three simulations performed with general circulation models and one carried out with LOVECLIM, a model of intermediate complexity. The conclusions derived from this analysis confirm

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Basu, Sayak, Sambit Ghosh, and Prasanta Sanyal. "Spatial heterogeneity in the relationship between precipitation and carbon isotopic discrimination in C3 plants: Inferences from a global compilation." Global and Planetary Change 176 (May 2019): 123–31. http://dx.doi.org/10.1016/j.gloplacha.2019.02.002.

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Larocca, Laura J., and Yarrow Axford. "Arctic glaciers and ice caps through the Holocene:a circumpolar synthesis of lake-based reconstructions." Climate of the Past 18, no. 3 (2022): 579–606. http://dx.doi.org/10.5194/cp-18-579-2022.

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Abstract. The recent retreat of nearly all glaciers and ice caps (GICs) located in Arctic regions is one of the most clear and visible signs of ongoing climate change. This paper synthesizes published records of Holocene GIC fluctuations from lake archives, placing their recent retreat into a longer-term context. Our compilation includes 66 lake-based GIC records (plus one non-lake-based record from the Russian Arctic) from seven Arctic regions: Alaska, Baffin Island in northeastern Canada, Greenland, Iceland, the Scandinavian peninsula, Svalbard, and the Russian high Arctic. For each region a

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Chimani, Barbara, Christoph Matulla, Johann Hiebl, et al. "Compilation of a guideline providing comprehensive information on freely available climate change data and facilitating their efficient retrieval." Climate Services 19 (August 2020): 100179. http://dx.doi.org/10.1016/j.cliser.2020.100179.

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19

Meister, Philip, Anne Alexandre, Hannah Bailey, et al. "A global compilation of diatom silica oxygen isotope records from lake sediment – trends and implications for climate reconstruction." Climate of the Past 20, no. 2 (2024): 363–92. http://dx.doi.org/10.5194/cp-20-363-2024.

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Abstract. Oxygen isotopes in biogenic silica (δ18OBSi) from lake sediments allow for quantitative reconstruction of past hydroclimate and proxy-model comparison in terrestrial environments. The signals of individual records have been attributed to different factors, such as air temperature (Tair), atmospheric circulation patterns, hydrological changes, and lake evaporation. While every lake has its own local set of drivers of δ18O variability, here we explore the extent to which regional or even global signals emerge from a series of paleoenvironmental records. This study provides a comprehens

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Reschke, Maria, Kira Rehfeld, and Thomas Laepple. "Empirical estimate of the signal content of Holocene temperature proxy records." Climate of the Past 15, no. 2 (2019): 521–37. http://dx.doi.org/10.5194/cp-15-521-2019.

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Abstract. Proxy records from climate archives provide evidence about past climate changes, but the recorded signal is affected by non-climate-related effects as well as time uncertainty. As proxy-based climate reconstructions are frequently used to test climate models and to quantitatively infer past climate, we need to improve our understanding of the proxy record signal content as well as the uncertainties involved. In this study, we empirically estimate signal-to-noise ratios (SNRs) of temperature proxy records used in global compilations of the middle to late Holocene (last 6000 years). Th

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Mairesse, A., H. Goosse, P. Mathiot, H. Wanner, and S. Dubinkina. "Investigating the consistency between proxy-based reconstructions and climate models using data assimilation: a mid-Holocene case study." Climate of the Past 9, no. 6 (2013): 2741–57. http://dx.doi.org/10.5194/cp-9-2741-2013.

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Abstract. The mid-Holocene (6 kyr BP; thousand years before present) is a key period to study the consistency between model results and proxy-based reconstruction data as it corresponds to a standard test for models and a reasonable number of proxy-based records is available. Taking advantage of this relatively large amount of information, we have compared a compilation of 50 air and sea surface temperature reconstructions with the results of three simulations performed with general circulation models and one carried out with LOVECLIM, a model of intermediate complexity. The conclusions derive

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Mohammadi, Forogh, Hossein Mahmoudi, Yasaman Ranjbaran, and Faraham Ahmadzadeh. "Compilation and prioritizing human-wildlife conflict management strategies using the WASPAS method in Iran." Environmental Challenges 7 (April 2022): 100482. http://dx.doi.org/10.1016/j.envc.2022.100482.

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Clark, Autumn S., Devan Allen McGranahan, Benjamin A. Geaumont, Carissa L. Wonkka, Jacqueline P. Ott, and Urs P. Kreuter. "Barriers to Prescribed Fire in the US Great Plains, Part I: Systematic Review of Socio-Ecological Research." Land 11, no. 9 (2022): 1521. http://dx.doi.org/10.3390/land11091521.

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Prescribed fire is increasingly being considered as a viable management tool by public and private land managers. Fully expanding prescribed fire use in a land management context, where it is an ecologically effective but not commonly applied tool, requires a comprehensive understanding of barriers that limit prescribed fire, especially in working rangelands of the North American Great Plains. While there is an emerging body of work on the perceptions of prescribed fire, there has yet to be a compilation of the research. We present a systematic review of the published literature on the percept

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Shah, Shwetal. "Book Review - Navroz K. Dubash, India in a Warming World – Integrating Climate Change and Development (New Delhi: Oxford University Press, 2019)." Liberal Studies 5, no. 1 (2020): 147–50. https://doi.org/10.5281/zenodo.4318655.

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In this book, Navroz Dubash has brought to its readers' various perspectives of different experts from the field of climate science and policy and created a comprehensive volume in order to understand the Indian perspective on <em>Climate Change</em>. It is one such comprehensive and authentic compilation and also the first on this subject after the crucial Paris Agreement in 2015, comprising of different articles by various experts. Moreover, this edited volume is beyond scientific facts of climate change and comprises important angles of social, political, and financial issues associated

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Kageyama, Masa, Louise C. Sime, Marie Sicard, et al. "A multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: sea ice data compilation and model differences." Climate of the Past 17, no. 1 (2021): 37–62. http://dx.doi.org/10.5194/cp-17-37-2021.

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Abstract. The Last Interglacial period (LIG) is a period with increased summer insolation at high northern latitudes, which results in strong changes in the terrestrial and marine cryosphere. Understanding the mechanisms for this response via climate modelling and comparing the models' representation of climate reconstructions is one of the objectives set up by the Paleoclimate Modelling Intercomparison Project for its contribution to the sixth phase of the Coupled Model Intercomparison Project. Here we analyse the results from 16 climate models in terms of Arctic sea ice. The multi-model mean

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Kageyama, Masa, Louise C. Sime, Marie Sicard, et al. "A multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: sea ice data compilation and model differences." Climate of the Past 17, no. 1 (2021): 37–62. http://dx.doi.org/10.5194/cp-17-37-2021.

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Abstract. The Last Interglacial period (LIG) is a period with increased summer insolation at high northern latitudes, which results in strong changes in the terrestrial and marine cryosphere. Understanding the mechanisms for this response via climate modelling and comparing the models' representation of climate reconstructions is one of the objectives set up by the Paleoclimate Modelling Intercomparison Project for its contribution to the sixth phase of the Coupled Model Intercomparison Project. Here we analyse the results from 16 climate models in terms of Arctic sea ice. The multi-model mean

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Baril, A., E. Garrett, G. A. Milne, W. R. Gehrels, and J. T. Kelley. "Postglacial relative sea-level changes in the Gulf of Maine, USA: Database compilation, assessment and modelling." Quaternary Science Reviews 306 (April 2023): 108027. http://dx.doi.org/10.1016/j.quascirev.2023.108027.

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S., B. Kanungo. "A compilation and critical evaluation of the literature data on thermal dehydration of hydrated salts." Journal of Indian Chemical Society Vol. 86, Jul 2009 (2009): 679–89. https://doi.org/10.5281/zenodo.5814105.

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Institute of Minerals and Materials Technology (Formerly R.R.L.), Bhubaneswar-751 013, Orissa, India <em>E-mail </em>: sbk_your@yahoo.co.in <em>Manuscript received 7 January 2008, revised 16 March 2009, accepted 17 March 2009</em> The article provides a detailed compilation of literature data on the thermal dehydration of simple (formed from single cation and anion) hydrated salts consisting of a wide variety of cations and anions or ligands. An attempt has been made to correlate the temperature and apparent activation energy of dehydration with either charge density (z/r) of cation or stabili

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Burke, Victoria, Doreen Richter, Ulrike Hass, Uwe Duennbier, Janek Greskowiak, and Gudrun Massmann. "Redox-dependent removal of 27 organic trace pollutants: compilation of results from tank aeration experiments." Environmental Earth Sciences 71, no. 8 (2013): 3685–95. http://dx.doi.org/10.1007/s12665-013-2762-8.

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Chen, M. T., C. C. Huang, U. Pflaumann, C. Waelbroeck, and M. Kucera. "Estimating glacial western Pacific sea-surface temperature: methodological overview and data compilation of surface sediment planktic foraminifer faunas." Quaternary Science Reviews 24, no. 7-9 (2005): 1049–62. http://dx.doi.org/10.1016/j.quascirev.2004.07.013.

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Moreno, Ana, Anders Svensson, Stephen J. Brooks, et al. "A compilation of Western European terrestrial records 60–8 ka BP: towards an understanding of latitudinal climatic gradients." Quaternary Science Reviews 106 (December 2014): 167–85. http://dx.doi.org/10.1016/j.quascirev.2014.06.030.

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Morrill, C., D. M. Anderson, B. A. Bauer, et al. "Proxy benchmarks for intercomparison of 8.2 ka simulations." Climate of the Past 9, no. 1 (2013): 423–32. http://dx.doi.org/10.5194/cp-9-423-2013.

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Abstract. The Paleoclimate Modelling Intercomparison Project (PMIP3) now includes the 8.2 ka event as a test of model sensitivity to North Atlantic freshwater forcing. To provide benchmarks for intercomparison, we compiled and analyzed high-resolution records spanning this event. Two previously-described anomaly patterns that emerge are cooling around the North Atlantic and drier conditions in the Northern Hemisphere tropics. Newer to this compilation are more robustly-defined wetter conditions in the Southern Hemisphere tropics and regionally-limited warming in the Southern Hemisphere. Most a

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Morrill, C., D. M. Anderson, B. A. Bauer, et al. "Proxy benchmarks for intercomparison of 8.2 ka simulations." Climate of the Past Discussions 8, no. 4 (2012): 3765–89. http://dx.doi.org/10.5194/cpd-8-3765-2012.

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Abstract. The Paleoclimate Modelling Intercomparison Project (PMIP3) now includes the 8.2 ka event as a test of model sensitivity to North Atlantic freshwater forcing. To provide benchmarks for intercomparison, we compiled and analyzed high-resolution records spanning this event. Two previously-described anomaly patterns that emerge are cooling around the North Atlantic and drier conditions in the Northern Hemisphere tropics. Newer to this compilation are more robustly-defined wetter conditions in the Southern Hemisphere tropics and regionally-limited warming in the Southern Hemisphere. Most a

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Klippel, Lara, Scott St. George, Ulf Büntgen, Paul J. Krusic, and Jan Esper. "Differing pre-industrial cooling trends between tree rings and lower-resolution temperature proxies." Climate of the Past 16, no. 2 (2020): 729–42. http://dx.doi.org/10.5194/cp-16-729-2020.

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Abstract. The new PAGES2k global compilation of temperature-sensitive proxies offers an unprecedented opportunity to study regional to global trends associated with orbitally driven changes in solar irradiance over the past 2 millennia. Here, we analyze pre-industrial long-term trends from 1 to 1800 CE across the PAGES2k dataset and find that, in contrast to the gradual cooling apparent in ice core, marine, and lake sediment data, tree rings do not exhibit the same decline. To understand why tree-ring proxies lack any evidence of a significant pre-industrial cooling, we divide those data by lo

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Vasiliki, Papaioannou, and Anagnou Evaggelos. "Evaluation of Greek Second Chance Schools in Prison by Detainees." Education Quarterly Reviews 3, no. 1 (2020): 10–22. https://doi.org/10.31014/aior.1993.03.01.114.

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  With the establishment of Second Chance Schools (SCS) inside Greek prisons, a more systematic and integrated effort was made for the overall development of trainees. Many studies have been conducted regarding the work that SCS provide. For this reason, a systematic review of the relevant bibliography and a compilation of the findings of the studies realized between 2006-2018, regarding the evaluation of the educational program provided by SCS in the prison, was considered appropriate. The results demonstrate that all inmate trainees evaluate SCS positively, concerning the educators, the

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Bolliet, Timothé, Patrick Brockmann, Valérie Masson-Delmotte, et al. "Water and carbon stable isotope records from natural archives: a new database and interactive online platform for data browsing, visualizing and downloading." Climate of the Past 12, no. 8 (2016): 1693–719. http://dx.doi.org/10.5194/cp-12-1693-2016.

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Abstract. Past climate is an important benchmark to assess the ability of climate models to simulate key processes and feedbacks. Numerous proxy records exist for stable isotopes of water and/or carbon, which are also implemented inside the components of a growing number of Earth system model. Model–data comparisons can help to constrain the uncertainties associated with transfer functions. This motivates the need of producing a comprehensive compilation of different proxy sources. We have put together a global database of proxy records of oxygen (δ18O), hydrogen (δD) and carbon (δ13C) stable

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Charman, Dan J., Antony Blundell, Richard C. Chiverrell, Dawn Hendon, and Pete G. Langdon. "Compilation of non-annually resolved Holocene proxy climate records: stacked Holocene peatland palaeo-water table reconstructions from northern Britain." Quaternary Science Reviews 25, no. 3-4 (2006): 336–50. http://dx.doi.org/10.1016/j.quascirev.2005.05.005.

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Fedorov, Alexander N., Pavel Y. Konstantinov, Nikolay F. Vasiliev, et al. "Ice Volumes in Permafrost Landscapes of Arctic Yakutia." Land 11, no. 12 (2022): 2329. http://dx.doi.org/10.3390/land11122329.

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This article is devoted to the study of the distribution of ground ice volumes in the upper layers of 5–10 m permafrost in the permafrost landscapes of Arctic Yakutia. Compilation of such a map will serve as a basis for assessing the vulnerability of permafrost to global warming, anthropogenic impact and forecasting the evolution of permafrost landscapes. The map was compiled using ArcGIS software, which supports attribute table mapping. The ground ice map of Arctic Yakutian permafrost landscapes shows that about 19% of the area is occupied by ultra ice-rich (above 0.6 in volumetric ice conten

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Annan, J. D., and J. C. Hargreaves. "A new global reconstruction of temperature changes at the Last Glacial Maximum." Climate of the Past 9, no. 1 (2013): 367–76. http://dx.doi.org/10.5194/cp-9-367-2013.

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Abstract. Some recent compilations of proxy data both on land and ocean (MARGO Project Members, 2009; Bartlein et al., 2011; Shakun et al., 2012), have provided a new opportunity for an improved assessment of the overall climatic state of the Last Glacial Maximum. In this paper, we combine these proxy data with the ensemble of structurally diverse state of the art climate models which participated in the PMIP2 project (Braconnot et al., 2007) to generate a spatially complete reconstruction of surface air (and sea surface) temperatures. We test a variety of approaches, and show that multiple li

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Annan, J. D., and J. C. Hargreaves. "A new global reconstruction of temperature changes at the Last Glacial Maximum." Climate of the Past Discussions 8, no. 5 (2012): 5029–51. http://dx.doi.org/10.5194/cpd-8-5029-2012.

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Abstract. Some recent compilations of proxy data both on land and ocean (MARGO Project Members, 2009; Bartlein et al., 2011; Shakun et al., 2012), have provided a new opportunity for an improved assessment of the overall climatic state of the Last Glacial Maximum. In this paper, we combine these proxy data with the ensemble of structurally diverse state of the art climate models which participated in the PMIP2 project (Braconnot et al., 2007) to generate a spatially complete reconstruction of surface air (and sea surface) temperatures. We test a variety of approaches, and show that multiple li

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Hessler, I., S. P. Harrison, M. Kucera, et al. "Implication of methodological uncertainties for Mid-Holocene sea surface temperature reconstructions." Climate of the Past Discussions 10, no. 2 (2014): 1747–82. http://dx.doi.org/10.5194/cpd-10-1747-2014.

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Abstract. We present and examine a~multi-sensor global compilation of Mid-Holocene (MH) sea surface temperatures (SSTs), based on Mg/Ca and alkenone palaeothermometry and reconstructions obtained using planktonic foraminifera and organic-walled dinoflagellate cyst census counts. We assess the uncertainties originating from using different methodologies and evaluate the potential of MH SST reconstructions as a benchmark for climate-model simulations. The comparison between different analytical approaches (time frame, baseline climate) shows the choice of time window for the MH has a negligible

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Dansereau, Pierre-René, and Yves Bergeron. "Fire history in the southern boreal forest of northwestern Quebec." Canadian Journal of Forest Research 23, no. 1 (1993): 25–32. http://dx.doi.org/10.1139/x93-005.

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Age determination of post-fire forests and the analysis of fire scars on surviving trees have allowed for the historical reconstruction and mapping of fires in a forest area of 11 715 ha in northwestern Quebec, south of Lake Abitibi. Most of the study area was burnt by two large fires (>1000 ha) in 1760 and 1923. All the other fires recorded (1797, 1823, 1870, 1907, 1919) were smaller in extent and occurred in a restricted part (1984 ha) of the study area, characterized by the fragmentation of the forest landscape by water bodies. The compilation of data concerning area burnt per type of su

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Prado, L. F., I. Wainer, C. M. Chiessi, M. P. Ledru, and B. Turcq. "A mid-Holocene climate reconstruction for eastern South America." Climate of the Past 9, no. 5 (2013): 2117–33. http://dx.doi.org/10.5194/cp-9-2117-2013.

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Abstract. The mid-Holocene (6000 calibrated years before present) is a key period in palaeoclimatology because incoming summer insolation was lower than during the late Holocene in the Southern Hemisphere, whereas the opposite happened in the Northern Hemisphere. However, the effects of the decreased austral summer insolation over South American climate have been poorly discussed by palaeodata syntheses. In addition, only a few of the regional studies have characterised the mid-Holocene climate in South America through a multiproxy approach. Here, we present a multiproxy compilation of mid-Hol

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Moreau, M., T. Corrège, E. P. Dassié, and F. Le Cornec. "Evidence for the non-influence of salinity variability on the <i>Porites</i> coral Sr/Ca palaeothermometer." Climate of the Past 11, no. 3 (2015): 523–32. http://dx.doi.org/10.5194/cp-11-523-2015.

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Abstract. Porites coral-based sea surface temperature (SST) reconstructions are obtained from the measurement of skeleton Sr/Ca ratio. However, the influence of salinity in the incorporation of these trace elements in the Porites aragonitic skeleton is still poorly documented. Laboratory experiments indicate that in three different coral species (not including the widely used Porites genus), salinity does not influence the Sr/Ca thermometer. In this study, we test the salinity effect on Porites Sr/Ca-based SST reconstructions at monthly and interannual timescales in open-ocean environmental co

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van der Boon, Annique, Klaudia F. Kuiper, Robin van der Ploeg, et al. "Exploring a link between the Middle Eocene Climatic Optimum and Neotethys continental arc flare-up." Climate of the Past 17, no. 1 (2021): 229–39. http://dx.doi.org/10.5194/cp-17-229-2021.

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Abstract. The Middle Eocene Climatic Optimum (MECO), a ∼500 kyr episode of global warming that initiated at ∼ 40.5 Ma, is postulated to be driven by a net increase in volcanic carbon input, but a direct source has not been identified. Here we show, based on new and previously published radiometric ages of volcanic rocks, that the interval spanning the MECO corresponds to a massive increase in continental arc volcanism in Iran and Azerbaijan. Ages of Eocene igneous rocks in all volcanic provinces of Iran cluster around 40 Ma, very close to the peak warming phase of the MECO. Based on the spatia

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Paasche, Ø., and J. Bakke. "Defining the Little Ice Age." Climate of the Past Discussions 6, no. 5 (2010): 2159–75. http://dx.doi.org/10.5194/cpd-6-2159-2010.

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Abstract. The "Little Ice Age" (LIA) is possibly the best-documented climatic anomaly of the past. A wide range of datasets portrays a harsh climate that worsened living conditions, primarily in terms of cooler temperatures, for people across Europe sometime during the last millennium. Regardless of the vast amount of data covering the LIA, there is presently no consensus concerning its spatial manifestation (was it regional or global?), its temporal constraints (when did it start and end?), or the broad-scale dynamics associated with it (what mechanisms did it involve?), although there is no

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Fuhrmann, Florian, Benedikt Diensberg, Xun Gong, Gerrit Lohmann, and Frank Sirocko. "Aridity synthesis for eight selected key regions of the global climate system during the last 60 000 years." Climate of the Past 16, no. 6 (2020): 2221–38. http://dx.doi.org/10.5194/cp-16-2221-2020.

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Abstract. A compilation of the published literature on dust content in terrestrial and marine sediment cores was synchronized with pollen data and speleothem growth phases on the Greenland Ice Core Chronology 2005 (GICC05) time axis. Aridity patterns for eight key areas of the global climate system have been reconstructed for the last 60 000 years. These records have different time resolutions and different dating methods, i.e. different types of stratigraphy. Nevertheless, all regions analysed in this study show humid conditions during early Marine Isotope Stage 3 (MIS3) and the early Holocen

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Kaiser Kudsk, Sabrina Gjødvad, Mads Faurschou Knudsen, Christoffer Karoff, Claudia Baittinger, Stergios Misios, and Jesper Olsen. "Solar variability between 650 CE and 1900 - Novel insights from a global compilation of new and existing high-resolution 14C records." Quaternary Science Reviews 292 (September 2022): 107617. http://dx.doi.org/10.1016/j.quascirev.2022.107617.

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Reeves, Jessica M., Timothy T. Barrows, Timothy J. Cohen, et al. "Climate variability over the last 35,000 years recorded in marine and terrestrial archives in the Australian region: an OZ-INTIMATE compilation." Quaternary Science Reviews 74 (August 2013): 21–34. http://dx.doi.org/10.1016/j.quascirev.2013.01.001.

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Bakker, P., and H. Renssen. "Last Interglacial model-data mismatch of thermal maximum temperatures partially explained." Climate of the Past Discussions 10, no. 1 (2014): 739–60. http://dx.doi.org/10.5194/cpd-10-739-2014.

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Abstract. The timing of the Last Interglacial (LIG) thermal maximum is highly uncertain. Compilations of maximum LIG temperatures are therefore based on the assumption that maximum warmth occurred synchronously across the globe. Although known to be an oversimplification, the impact of this assumption on temperature estimates has yet to be assessed. We use the LIG temperature evolutions simulated by 9 different climate models to investigate whether the assumption of synchronicity results in a sizeable overestimation of LIG thermal maximum temperatures. We find that for annual temperatures, the

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