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Letteratura scientifica selezionata sul tema "Paleoclimatology"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 29 luglio 2024

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Articoli di riviste sul tema "Paleoclimatology"

Andrews, John T. "Paleoclimatology". Palaeogeography, Palaeoclimatology, Palaeoecology 111, n. 1-2 (settembre 1994): 180–81. http://dx.doi.org/10.1016/0031-0182(94)90359-x.

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Holser, William T. "Paleoclimatology". Geochimica et Cosmochimica Acta 57, n. 7 (aprile 1993): 1635. http://dx.doi.org/10.1016/0016-7037(93)90023-p.

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Stokes, Stephen. "Paleoclimatology - even better!" Journal of Biogeography 27, n. 2 (marzo 2000): 501. http://dx.doi.org/10.1046/j.1365-2699.2000.00413.x.

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Nieto-Barajas, Luis Enrique. "Interpolation of paleoclimatology datasets". Atmósfera 31, n. 2 (1 aprile 2018): 125–41. http://dx.doi.org/10.20937/atm.2018.31.02.02.

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KANO, Akihiro. "Perspectives in carbonate paleoclimatology". Japanese Magazine of Mineralogical and Petrological Sciences 33, n. 3 (2004): 136–40. http://dx.doi.org/10.2465/gkk.33.136.

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CROWLEY, T. J. "Paleoclimatology: Milankovitch and Climate." Science 227, n. 4688 (15 febbraio 1985): 745–46. http://dx.doi.org/10.1126/science.227.4688.745-a.

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Oppo, D. "PALEOCLIMATOLOGY: Millennial Climate Oscillations". Science 278, n. 5341 (14 novembre 1997): 1244–46. http://dx.doi.org/10.1126/science.278.5341.1244.

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Eglinton, Timothy I., e Geoffrey Eglinton. "Molecular proxies for paleoclimatology". Earth and Planetary Science Letters 275, n. 1-2 (ottobre 2008): 1–16. http://dx.doi.org/10.1016/j.epsl.2008.07.012.

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Idso, S. B. "A Problem for Paleoclimatology?" Quaternary Research 31, n. 3 (maggio 1989): 433–34. http://dx.doi.org/10.1016/0033-5894(89)90051-3.

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Webb, Robert S., Jonathan T. Overpeck, David M. Anderson, Bruce A. Bauer, Mildred K. England, Wendy S. Gross, E. Ann Meyers e Michael M. Worobec. "World Data Center-A for Paleoclimatology at the NOAA Paleoclimatology Program, Boulder, CO". Journal of Paleolimnology 9, n. 1 (1993): 69–75. http://dx.doi.org/10.1007/bf00680037.

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Più fonti

Tesi sul tema "Paleoclimatology"

Griffin, Richard Daniel. "North American Monsoon Paleoclimatology From Tree Rings". Diss., The University of Arizona, 2013. http://hdl.handle.net/10150/301558.

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The North American monsoon is central to Southwestern climate and is a research focus in climatology. Of the various monsoon paleoclimate proxies, precisely dated and seasonally resolved tree-ring records offer unique opportunity for contextualizing modern instrumental observations and climate model projections. Focused on latewood, the dark-colored sub-annual component of conifer tree rings that forms in the late growing season, this dissertation research represents a systematic effort to diagnose the tree-growth response to monsoon climate, to develop a replicated network of monsoon-sensitive chronologies, and to characterize monsoon paleoclimate variability in the southwestern United States. A pilot study using latewood measurements from five locations assessed seasonal climate response sensitivity to various chronology development techniques. Results informed a protocol for chronology development, which was used to produce a unique network of 53 monsoon-sensitive latewood chronologies for the southwestern United States. A chronology subset was used to develop the first monsoon precipitation reconstruction for a large and important region of the southwestern United States and northwestern Mexico. This reconstruction revealed monsoon paleodroughts more persistent and extreme than any during the instrumental era and indicated that the southwestern decadal droughts of the last 470 years were characterized not just by cool-season precipitation deficits, but also by persistently dry monsoon conditions. The previously noted tendency for winter and summer precipitation to be out of phase was found to be unstable through time and anomalously strong during the recent instrumental era. The paleoclimatic significance of the new sub-annual chronology network was characterized in terms of chronology signal strength, climate response seasonality, and dominant spatiotemporal structure. With only a few exceptions, the latewood chronologies were found to contain monsoon-specific climate signal that was not available from previously existing records of annual tree-ring width. Principal components analysis revealed that the chronology network captures both temporal variability and spatial structure inherent to monsoon precipitation. As such, proxy data developed in this dissertation are unique are uniquely suited for studying spatiotemporal variability in monsoon paleoclimate. Outcomes from this dissertation are broadly relevant in environmental research and could potentially inform long-term strategies for adaptive management of natural resources.

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Cisneros, Bermejo Mercè. "Reconstrucció climàtica dels darrers 2.700 anys a la Mediterrània occidental: sediments marins i estalagmites". Doctoral thesis, Universitat de Barcelona, 2019. http://hdl.handle.net/10803/668453.

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Donada l’alta sensibilitat de la regió central de la Mediterrània occidental a la variabilitat climàtica, s’han reconstruït les condicions de la mar superficials i profundes així com de les atmosfèriques pels darrers 2.700 anys. Les condicions marines han estat reconstruïdes a partir de multi-testimonis de sediment del nord de Menorca i les condicions atmosfèriques (hidroclimàtiques) en base a cinc registres d’espeleotemes de dues coves de Mallorca. La integració de la informació derivada d’aquests dos tipus d’arxius ha permès un millor enteniment de la interacció entre la mar superficial i profunda i l’atmosfera. Els principals períodes climàtics/històrics caracteritzats són: Període Talaiòtic (TP; fins el 123 BCE), Període Romà (RP; 123 BCE-470 CE(1)), Alta Edat Mitjana (EMA; 470 a 900 CE), Anomalia Climàtica Medieval (MCA; 900 a 1275 CE) i Petita Edat de Gel (LIA; 1275 a 1850 CE). Les Temperatures de la Mar Superficial (SST) s’han obtingut a partir de la ràtio Mg/Ca analitzada al foraminífer planctònic Globigerina bulloides (Cisneros et al., 2016), re- ajustant el calibratge de les SST per a la Mediterrània Occidental. La intensitat dels corrents fondos s’ha reconstruït a partir d’anàlisis de la mida de gra (paràmetre UP10, fracció >10 µm; Cisneros et al., 2019). Aquest paràmetre UP10 ha estat revalidat amb dades oceanogràfiques mostrejades durant els anys 2012-2014 mitjançant dos ancoratges instrumentats d’aigües profundes. La variabilitat hidroclimàtica ha estat reconstruïda emprant una metodologia que integra varis indicadors (anàlisi geoquímics i texturals) a les estalagmites. El període càlid més sostingut va tenir lloc durant el RP, el qual és seguit per una tendència de refredament interrompuda per vàries oscil·lacions a escala de centennis. Tot i que alguns períodes amb SST particularment càlides van tenir lloc durant la MCA, la LIA va estar marcadament inestable, amb alguns esdeveniments molt freds sobretot durant la segona meitat del període. Els esdeveniments més forts de formació d’aigua fonda van ocórrer durant intervals relativament càlids, com el RP, el final de la MCA i la primera part de la LIA. Per contra, les dades indiquen una reducció progressiva de la convecció durant l’EMA, resultant en esdeveniments durant la major part de la MCA. Els registres obtinguts de les estalagmites ha permès elaborar la primera reconstrucció regional de la variabilitat hidroclimàtica pels darrers 2.700 anys. Els registres indiquen condicions generalment humides per l’inici del RP, la primera meitat de l’EMA i per tota la LIA, en contrast amb les condicions més seques enregistrades pel RP tardà (anys 200-470 CE), la segona part de l’EMA (anys 700-900 CE) i tota la MCA. Dins de la LIA, al voltant de l’any 1622 CE, la existència d’un nivell detrític, enriquit en Ti a l’estalagmita Seán ha estat interpretat com un marcador d’inundacions associat a un esdeveniment extrem de pluja. La combinació integrada dels resultats derivats dels sediments marins i de les estalagmites suggereix condicions climàtiques no-estacionàries durant cadascun dels períodes estudiats dels últims 2.700 anys. Particularment durant el final del RP i la primera meitat de l’EMA, aquesta tesi suggereix una variabilitat climàtica més complexa i/o de més alta freqüència. L’EMA sembla haver estat caracteritzat com un període transició i, haver estat previ a una re-configuració atmosfèrica de diferents modes climàtics com el patró East Atlantic/West Russian i l’Oscil·lació de l’Atlàntic Nord. (1) BCE: anys abans de l’era comú/CE: anys de l’era comú
Surface-deep ocean and atmospheric reconstructions for the last 2.7 kyr have been performed taking the advantage of the high sensitivity of the central-western Mediterranean region. Ocean conditions have been reconstructed from sediment multicores recovered in the North Minorca and atmospheric conditions (hydroclimate) from five speleothem records of two Mallorca caves. The integration of this information has allowed a better understanding about the interaction between the surface-deep-sea and the atmosphere. The main climate/historical periods characterized are: Talaiotic Period (until 123BCE(1)), Roman Period (RP; 123BCE-470CE), Early Middle Ages (EMA; 470-900CE), Medieval Climate Anomaly (MCA; 900-1275CE) and Little Ice Age (LIA; 1275-1850CE). Sea-surface temperatures are derived from Mg/Ca-ratios analysed on planktonic foraminifera Globigerina bulloides (Cisneros et al., 2016) and deep-current intensity- changes from grain-size analysis (UP10-fraction; Cisneros et al., 2019). Hydroclimate variability has been reconstructed applying a multi-proxy approach (geochemical and textural analyses) on the stalagmites. The warmest sustained period occurred during the RP, followed by a general cooling trend interrupted by several centennial-scale oscillations. Although warm intervals took place during the MCA, the LIA was markedly unstable, with some very cold events mostly during its second half. The strongest deep-water formation events occurred during relatively warm intervals, such as the RP, the end of the MCA and the first part of the LIA. By contrast, our data indicate a progressive reduction in the overturning conditions during the EMA resulting in weaker deep-water formation events during most of the MCA. General wet conditions have been obtained for the early RP, the first half of the EMA and the entire LIA while drier conditions have characterized the late RP, the late EMA and the entire MCA. The combination of the results derived from marine sediments and stalagmites suggests non-stationary climate conditions during each period of the last 2.7 kyr. Particularly during the late RP and the first half of the EMA, more complex climate variability and/or with higher frequency seems to have occurred. The EMA seems to have been characterized like a transition period, previous to an atmospheric reconfiguration of different climate modes such as the East Atlantic/West Russian and NAO. (1) BCE: Before Common Era years/CE: Common Era years

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Maier, Éder Leandro Bayer. "Relações espaço-temporais entre dados paleoclimáticos do Nevado Illimani (Bolívia) e a precipitação na América do Sul". reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2014. http://hdl.handle.net/10183/94677.

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Este trabalho investiga a possibilidade de reconstruir a variabilidade da precipitação pretérita na América do Sul a partir de uma série temporal de razão isotópica de oxigênio (δ18O) em um testemunho de gelo obtido na Bolívia, para isso é analisado as relações espaço-temporais entre a precipitação sobre a América do Sul e a série do δ18O. Utilizou-se dados do δ18O dos primeiros 50 metros do testemunho de gelo do Nevado Illimani (6.350 m, 16º37’S, 67º46’W) e totais mensais da precipitação coletada em 890 estações meteorológicas sobre o continente sul-americano no período 1979–2008. As amostras da precipitação foram dispostas em uma grade equiespaçada com resolução de ~2º de latitude e longitude. A variabilidade espacial e temporal da precipitação foram analisadas pela Análise das Componentes Principais no Modo T e S, respectivamente, com a identificação dos principais Padrões Espaciais Anômalos (PEA) e das zonas espaciais em que a variação temporal das anomalias da precipitação é correlacionada. No núcleo de cada zona foi selecionada uma série temporal anômala da precipitação para comparar com a série do δ18O. Constatou-se que há 12 PEA da precipitação e que são originários, predominantemente, da variação na temperatura superficial dos oceanos Pacífico Equatorial e Atlântico Tropical Norte e 8 zonas espaciais em que a variação da precipitação é parcialmente homogênea. Analisando características dos PEA da precipitação com a variação do δ18O constata-se que os registros de máximo (mínimo) fracionamento isotópico no verão estão relacionados à seca (chuvas acima da média) na Amazônia ou no nordeste brasileiro. Já no inverno, os registros de máximo (mínimo) fracionamento isotópico estão relacionados a secas (chuvas acima da média no litoral) na região tropical e chuvas acima da média (secas) na região extratropical. O índice de correlação entre todas séries de precipitação com a série do δ18O mostrou que a variação sincronizada das variáveis altera-se sazonalmente em função da migração espacial dos mecanismos de transporte e convergência da umidade. A comparação das séries de precipitação das 8 zonas com o δ18O possibilitou identificar possíveis áreas para a reconstrução paleoclimática. Nas regiões equatorial e subtropical foi testado a reconstrução. Nessas áreas, os fatores que controlam as duas variáveis são os mesmos, predominando os oceanos Pacífico Equatorial e Atlântico Norte nas alterações das séries temporais com frequência entre 24 e 60 meses. Para reconstrução da variabilidade da precipitação pretérita a partir da variação do δ18O foram testada duas técnicas, uma utilizando a análise de dependência por regressão e outra pela adoção de PEA para casos específicos da variação do δ18O. A primeira técnica não gerou resultados satisfatórios, por isso não foi usada. Com a segunda técnica foi possível identificar com 80% de chance de acerto as secas na Amazônia, no nordeste brasileiro e na região subtropical e com 68% de chance de acerto as chuvas acima da média na região subtropical, quando a avaliação não considera a magnitude das anomalias da precipitação. Por outro lado, a técnica é limitada, porque os PEAs adotados como referência não representam a grande variabilidade da precipitação nessas regiões.
This thesis investigates the possibility of reconstructing the South American past precipitation variability based on an oxygen isotope ratio (δ18O) time series from a Bolivian ice core, for this we analysed the spatial-temporal relations between these two variables. We used δ18O data from the upper 50 meters of Nevado Illimani ice core (6,350 m, 16°37'S, 67°46'W) and monthly total precipitation collected at 890 weather stations in South America in the period 1979–2008. Precipitation samples were arranged in an equally spaced grid with a ~2° latitude and longitude. The precipitation temporal and spatial variability were analysed by Principal Component Analysis on Mode S and T, respectively, with the identification of the main Anomalous Spatial Patterns (ASP) and spatial zones in which temporal rainfall anomalies variations are correlated. At each zone core, we selected one anomalous precipitation time series to compare with the δ18O series. There are 12 precipitations ASP that originate predominantly from surface temperature variations in the equatorial Pacific and tropical North Atlantic oceans, and 8 spatial zones in which the precipitation variation is partially homogeneous. Analysing the precipitation ASP characteristics with the δ18O variation, it is observed that records of maximum (minimum) isotopic fractionation in summer are related to droughts (above average precipitations) in the Amazon and northeastern Brazil. In the winter, records of maximum (minimum) isotopic fractionation are related to droughts (above average rainfall in the coastal area) in the tropical region and above average rainfall (droughts) in the extratropical region. The correlation index among all series of precipitation with δ18O series showed that these variables synchronized variation alters seasonally depending on the transport mechanisms spatial migration and on the moisture convergence. The comparison of the 8 precipitation zones with the δ18O series enabled us to identify possible areas for paleoclimatic reconstruction, which are the equatorial and subtropical regions. In these areas, the factors controlling the two variables are the same, prevailing the equatorial Pacific and the North Atlantic changes in time series with frequency from 24 to 60 months. To reconstruct the precipitation variability from the past δ18O variation we tested two techniques, one using dependency analysis for regression and other adopting ASP for specific cases of δ18O variations. The first technique yielded no satisfactory results, so it was disregarded. Using the second technique, it was possible to identify droughts in Amazonia, the Brazilian northeast and in the subtropical region with 80% changes of success. Above the average rainfalls in the subtropical region are identify with 68% changes of success, if this assessment does not consider the magnitude of the precipitation anomalies. On the other hand, the technique has limitations because the ASPs adopted as reference do not represent the wide precipitation variability in these regions.

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Anchukaitis, Kevin John. "A Stable Isotope Approach to Neotropical Cloud Forest Paleoclimatology". Diss., The University of Arizona, 2007. http://hdl.handle.net/10150/195637.

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Many tropical trees do not form reliable annual growth rings, making it a challenge to develop tree-ring width chronologies for application to paleoclimatology in these regions. Here, I seek to establish high-resolution proxy climate records from trees without rings from the Monteverde Cloud Forest in Costa Rica using stable isotope dendroclimatology. Neotropical cloud forest ecosystems are associated with a relatively narrow range of geographic and hydroclimatic conditions, and are potentially sensitive to climate variability and change at time scales from annual to centennial and longer. My approach takes advantage of seasonal changes in the d18O of water sources used by trees over a year, a signature that is imparted to the radial growth and provides the necessary chronological control. A rapid wood extraction technique is evaluated and found to produce cellulose with d18O values indistinguishable from conventional approaches, although its application to radiocarbon requires a statistical correction. Analyses of plantation-grown Ocotea tenera reveal coherent annual d18O cycles up to 9 permil. The width of these cycles corresponds to observed basal growth increments. Interannual variability in d18O at this site is correlated with wet season precipitation anomalies. At higher elevations within the orographic cloud bank, year-to-year changes in the amplitude of oxygen isotope cycles show a relationship with dry season climate. Longer d18O chronologies from mature Pouteria (Sapotacae) reveal that dry season hydroclimatology is controlled at interannual time scales by variability in the eastern equatorial Pacific (ENSO) and the Western Hemisphere Warm Pool (WHWP), which are correlated with trade wind strength and local air temperature. A change in the late 1960s toward enhanced annual d18O amplitude may reflect low frequency changes in the Atlantic and Pacific ocean-atmosphere system. This study establishes the basis for cloud forest isotope dendroclimatology and demonstrates that the local climate of neotropical cloud forests is sensitive to interannual, and perhaps, multidecadal changes in important large-scale modes of climate variability.

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Serefiddin, Feride Schwarcz H. P. "Paleoclimate models for western North America as inferred from speleothem isotope records /". *McMaster only, 2003.

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Wilhelms, Frank. "Messung dielektrischer Eigenschaften polarer Eiskerne = Measuring the dielectric properties of polar ice cores /". Bremerhaven : Alfred-Wegener-Institut für Polar- und Meeresforschung, 2000. http://www.gbv.de/dms/bs/toc/319750515.pdf.

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Dibenedetto, Joseph Nicholas. "Paleoclimatological implications of fossil tortoise bones". To access this resource online via ProQuest Dissertations and Theses @ UTEP, 2008. http://0-proquest.umi.com.lib.utep.edu/login?COPT=REJTPTU0YmImSU5UPTAmVkVSPTI=&clientId=2515.

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Sandau, Stephen D. "The Paleoclimate and Paleoecology of a Uintan (Late Middle Eocene) flora and fauna from the Uinta Basin, Utah /". Diss., CLICK HERE for online access, 2005. http://contentdm.lib.byu.edu/ETD/image/etd719.pdf.

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Minckley, Thomas A. "Holocene environmental history of the northwestern Great Basin and the analysis of modern pollen analogues in western North America /". view abstract or download file of text, 2003. http://wwwlib.umi.com/cr/uoregon/fullcit?p3113019.

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Thesis (Ph. D.)--University of Oregon, 2003.
Typescript. Includes vita and abstract. Includes bibliographical references (leaves 294-310). Also available for download via the World Wide Web; free to University of Oregon users.

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Rubio, de Inglés María Jesús. "Late Holocene Climate Variability in the North Atlantic based on biomarker reconstruction: The lake Azul (São Miguel, Azores archipielago) case". Doctoral thesis, Universitat de Barcelona, 2016. http://hdl.handle.net/10803/402145.

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The principal objective of this PhD thesis is to obtain a high resolution reconstruction of the climate (temperature and precipitation) in the north Atlantic for the late Holocene. This new reconstruction is from a sedimentary lacustrine record located in Azores (Lake Azul) that has been compared and discussing with principal other climate reconstructions published on the North Atlantic region. Climate in the North Atlantic is modulated by the conjunction of atmospheric patterns and ocean dynamics. The main atmospheric pattern is the North Atlantic Oscillation (NAO) but, other climatic modes such as the Eastern Atlantic (EA) and the Atlantic Meridional Oscillation (AMO) are also present. The use of biomarkers has appeared as a cutting edge technique to reconstruct climate and their validity has been proved by previous works. The Azul lacustrine sedimentary sequence occupied the last 660 years, and on it has been applied a multiproxy study including: facies analysis, X-Ray Diffraction (XRD), X-Ray Fluorescense (XRF), Total Organic Carbon (TOC), Total Nitrogen (TN), bulk isotopes of Carbon (δ13C) and Nitrogen (δ15N) and biomarkers (GDGTs and δD leaf waxes). Facies were grouped in two main facies types according to the velocity of sedimentation and the organic matter origin: (1) “Continuous facies” accumulated by a more or less continuously sedimentation processes and dominated by lake organic matter, and (2) “rapid facies” deposited from flood events and transporting mainly terrestrial organic matter. An accurate age-depth model based on 14C and 210Pb dates and XRF data was built to figure out those sudden changes (the Dynamic Age Model, DAM). The DAM calculates the age of the samples redistributing the time along the profile according to the amount of crystalline terrestrial particulated material. DAM can acquire short and long-term sedimentation rate (SR) changes and previous models only acquire long- term fluctuations. The biomarkers (GDGTs and δD leaf waxes) were extracted and studied on the continuous lacustrine facies to reconstruct temperature and precipitation. The relative percentage of GDGTs was transferred into temperature by the use of Pearson et al., (2011) calibration. The climatic factor affecting δD fractionation was assessed by the weekly collection of rain water showing a clear depletion with the amount of precipitation. Results from realized reconstruction suggested a climatic model that converge oceanic currents with the principal atmospheric patterns, defining the NAO as the main factor triggering the others. The temperature in Azores depends on the position of the Gulf Stream (GS). A positive (negative) NAO phase enhances (reduces) the Gulf Stream (GS) velocity that increases (reduce) the amount of Eddies around Bermuda driving towards north (east) the GS and heating up high (medium) latitudes. Therefore, a negative phase of NAO favors the GS heat to reach Azores. Since the temperature in Azores is modulated by the oceanic circulation, the AMO also plays an important role. The AMO is reflected in Ponta Delgada by the amplitude between maximum and minimum mean annual temperatures, which means an increase on seasonality. The AMO positive phase is reflected as an increase on temperatures in Lake Azul reconstruction. Otherwise, the AMO negative phase is masked by other climatic patterns. The precipitation in Azores is mainly triggered by the NAO phase, increasing (decreasing) precipitation during NAO negative (positive). The comparison with other reconstructions in the North Atlantic area suggested that an increase of precipitation in São Miguel produces an increase at other Azorean islands, the Iberian Peninsula and Morocco. This pattern has been observed for the last 700 years except for the period comprised between 1680 and 1920 AD where a possible southeastern shift of the NAO south dipole seemed to be produced. We suggest that this movement is produced by the occurrence, simultaneously, of an in phase and positive NAO and EA conjunction.

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Più fonti

Libri sul tema "Paleoclimatology"

Ramstein, Gilles, Amaëlle Landais, Nathaelle Bouttes, Pierre Sepulchre e Aline Govin, a cura di. Paleoclimatology. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-24982-3.

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R, North Gerald, a cura di. Paleoclimatology. New York: Oxford University Press, 1991.

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Crowley, Thomas J. Paleoclimatology. New York: Oxford University Press, 1996.

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Bradley, Raymond S. Quaternary paleoclimatology. New York: Chapman & Hall, 1997.

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Hönisch, Bärbel, Stephen M. Eggins, Laura L. Haynes, Katherine A. Allen, Katherine D. Holland e Katja Lorbacher. Boron Proxies in Paleoceanography and Paleoclimatology. Chichester, UK: John Wiley & Sons, Ltd, 2019. http://dx.doi.org/10.1002/9781119010678.

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Saltzman, Barry. Dynamical paleoclimatology: Generalized theory of global climate change. San Diego, Calif: Academic, 2002.

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Saltzman, Barry. Dynamical paleoclimatology: Generalized theory of global climate change. San Diego, Calif: Academic, 2002.

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National Seminar on Antarctic Geoscience, Ocean-atmosphere Interaction and Paleoclimatology (2003 Velha Goa, India). Antarctic geoscience, ocean-atmosphere interaction and paleoclimatology. A cura di Rajan S, Pandey Prem Chand e National Centre for Antarctic & Ocean Research (India). Goa: National Centre for Antarctic & Ocean Research, 2012.

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Esper, Jan. Paläoklimatische Untersuchungen an Jahrringen im Karakorum und Thien [sic] Shan Gebirge (Zentralasien). Sankt Augustin: In Kommission bei Asgard-Verlag, 2000.

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Survey), PRISM Project (Geological, e Geological Survey (U.S.), a cura di. PRISM 8p0s x 10p0s northern hemisphere paleoclimate reconstruction: Digital data. [Reston, Va.]: Dept. of the Interior, U.S. Geological Survey, 1994.

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Capitoli di libri sul tema "Paleoclimatology"

Southon, J. R., R. De Pol-Holz e E. R. M. Druffel. "Paleoclimatology". In Radiocarbon and Climate Change, 221–52. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-25643-6_7.

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Peterson, Larry C. "Paleoclimatology". In Encyclopedia of Earth Sciences Series, 1–14. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-39193-9_129-1.

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Peterson, Larry C. "Paleoclimatology". In Encyclopedia of Earth Sciences Series, 1147–60. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-39312-4_129.

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Patterson, William R. "Paleoclimatology". In The Palgrave Encyclopedia of Global Security Studies, 1–6. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-319-74336-3_427-1.

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Patterson, William R. "Paleoclimatology". In The Palgrave Encyclopedia of Global Security Studies, 1091–96. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-319-74319-6_427.

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Bowen, R. "Isotopic Paleoclimatology". In Nuclear Methods in Mineralogy and Geology, 453–93. Boston, MA: Springer US, 1998. http://dx.doi.org/10.1007/978-1-4615-5363-2_10.

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Bowen, R. "Isotopic Paleoclimatology". In Handbook of Nuclear Chemistry, 727–60. Boston, MA: Springer US, 2011. http://dx.doi.org/10.1007/978-1-4419-0720-2_16.

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Frakes, L. A. "Paleogeography and Paleoclimatology". In Cretaceous Resources, Events and Rhythms, 197–202. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-015-6861-6_10.

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Kageyama, Masa, e Didier Paillard. "Modeling and Paleoclimatology". In Frontiers in Earth Sciences, 319–42. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-24982-3_25.

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Bradley, Raymond S. "High-Resolution Paleoclimatology". In Dendroclimatology, 3–15. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-5725-0_1.

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Atti di convegni sul tema "Paleoclimatology"

Larose, Kayleen Mary. "FLOODING AND PALEOCLIMATOLOGY OF CENTRAL NEW HAMPSHIRE WETLANDS". In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-339350.

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Gill, Thomas E., e Joe D. Collins. "PROFESSIONAL DEVELOPMENT WORKSHOPS AS A FORCE MULTIPLIER: AN EXAMPLE FROM PALEOCLIMATOLOGY". In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-298691.

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Munoz, Samuel. "FLOODPLAIN LAKES AS A ROSETTA STONE FOR PALEOHYDROLOGY, PALEOECOLOGY, AND PALEOCLIMATOLOGY". In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321347.

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Barclay, Rich, Benjamin Lloyd, Regan Dunn, Ellen Currano, Ayuni Mohamaad, Kymbre Skersies e Surangi Punyasena. "CUTICLETRACE: A TOOLKIT FOR CAPTURING CELL OUTLINES OF LEAF CUTICLE WITH IMPLICATIONS FOR PALEOECOLOGY AND PALEOCLIMATOLOGY". In GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-393643.

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Ivory, Sarah, Philip Barker, Andrew S. Cohen, Ishmael Kimirei, Christine S. Lane, Melanie Leng, Michael M. McGlue et al. "LAKE TANGANYIKA DRILLING: ADDRESSING WORLD-CLASS SCIENTIFIC QUESTIONS IN PALEOCLIMATOLOGY, TECTONICS, AND EVOLUTIONARY ECOLOGY IN AFRICA’S OLDEST LAKE". In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303426.

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Lensky‬‏, Nadav G., Ido Sirota e Yehouda Enzel. "TEMPERATURE SEASONALITY CONTROL OVER MODERN HALITE LAYERS IN THE DEAD SEA: IN SITU OBSERVATIONS AND IMLICATIONS TO PALEOHYDROLOGY AND PALEOCLIMATOLOGY". In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300897.

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Ludvigson, Gregory, Andreas MÃ¶ller, Noah M. McLean, Marina B. Suarez e Jon Smith. "A NEW FRONTIER IN DEEP-TIME PALEOCLIMATOLOGY REGARDING THE GEOCHRONOLOGY OF PALEOSOLS: A TRIBUTE TO THE CAREER OF STEVEN DRIESE". In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-379387.

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Ludvigson, Greg A., Luis A. Gonzalez, R. M. Joeckel, Marina B. Suarez, Andreas Möller e Jeffrey B. Ross. "EXPLORING THE FRONTIER OF TERRESTRIAL APTIAN-ALBIAN (CRETACEOUS) C-ISOTOPE STRATIGRAPHY AND PALEOCLIMATOLOGY: A TRIBUTE TO THE SCIENTIFIC CAREER OF MICHAEL A. ARTHUR". In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-281223.

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Tafoya, A. J., L. J. Crossey, K. E. Karlstrom, M. Kolomaznik, V. Polyak, Y. Asmerom, S. A. Kelley e C. Cox. "Uranium-series dating of travertines from Soda Dam, New Mexico: Constructing a history of deposition, with implications for landscape evolution, paleohydrology, and paleoclimatology". In 2011 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2011. http://dx.doi.org/10.56577/sm-2011.610.

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Tafoya, A. J., L. J. Crossey, K. E. Karlstrom, V. Polyak, Y. Asmerom e C. Cox. "Uranium-series dating of travertine from Soda Dam, New Mexico: Constructing a history of deposition, with implications for landscape evolution, paleohydrology, and paleoclimatology". In 2012 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2012. http://dx.doi.org/10.56577/sm-2012.163.

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Rapporti di organizzazioni sul tema "Paleoclimatology"

Clague, J. J., e G. M. Macdonald. Paleoecology and paleoclimatology [Chapter 1: Quaternary geology of the Canadian Cordillera]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127943.

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Steig, E. J. Beryllium-10 in the Taylor Dome ice core: Applications to Antarctic glaciology and paleoclimatology. Office of Scientific and Technical Information (OSTI), dicembre 1996. http://dx.doi.org/10.2172/527444.

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White, J. M., T. A. Ager, D. P. Adam, E. B. Leopold, G. Liu, H. Jetté e C E Schweger. Neogene and Quaternary quantitative palynostratigraphy and paleoclimatology from sections in Yukon and adjacent Northwest Territories and Alaska. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1999. http://dx.doi.org/10.4095/210923.

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Chandler, F. W. Sedimentology and Paleoclimatology of the Huronian [Early Aphebian] Lorrain and Gordon Lake Formations and Their Bearing On Models For Sedimentary Copper Mineralization. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/120358.

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White, J. M. Palynology, age, correlation and paleoclimatology from JAPEX/JNOC/GSC Mallik 2L-38 gas hydrate research well and the significance for gas hydrates: a new approach. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/222149.

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White, J. M. Palynology, age, correlation, and paleoclimatology from JAPEX/JNOC/GSC Mallik 2L-38 gas hydrate research well and the significance for gas hydrate: a new approach. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2009. http://dx.doi.org/10.4095/247351.

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[Paleoclimatology studies for Yucca Mountain site characterization]. Final report. Office of Scientific and Technical Information (OSTI), maggio 1996. http://dx.doi.org/10.2172/631157.

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