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  • Carbon  (2)
  • Oceanographic data  (2)
  • Sea level  (2)
  • Thermohaline circulation  (2)
  • 2005-2009  (7)
  • 1955-1959
  • 1
    Publication Date: 2009-03-07
    Description: Amazon forests are a key but poorly understood component of the global carbon cycle. If, as anticipated, they dry this century, they might accelerate climate change through carbon losses and changed surface energy balances. We used records from multiple long-term monitoring plots across Amazonia to assess forest responses to the intense 2005 drought, a possible analog of future events. Affected forest lost biomass, reversing a large long-term carbon sink, with the greatest impacts observed where the dry season was unusually intense. Relative to pre-2005 conditions, forest subjected to a 100-millimeter increase in water deficit lost 5.3 megagrams of aboveground biomass of carbon per hectare. The drought had a total biomass carbon impact of 1.2 to 1.6 petagrams (1.2 x 10(15) to 1.6 x 10(15) grams). Amazon forests therefore appear vulnerable to increasing moisture stress, with the potential for large carbon losses to exert feedback on climate change.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Phillips, Oliver L -- Aragao, Luiz E O C -- Lewis, Simon L -- Fisher, Joshua B -- Lloyd, Jon -- Lopez-Gonzalez, Gabriela -- Malhi, Yadvinder -- Monteagudo, Abel -- Peacock, Julie -- Quesada, Carlos A -- van der Heijden, Geertje -- Almeida, Samuel -- Amaral, Ieda -- Arroyo, Luzmila -- Aymard, Gerardo -- Baker, Tim R -- Banki, Olaf -- Blanc, Lilian -- Bonal, Damien -- Brando, Paulo -- Chave, Jerome -- de Oliveira, Atila Cristina Alves -- Cardozo, Nallaret Davila -- Czimczik, Claudia I -- Feldpausch, Ted R -- Freitas, Maria Aparecida -- Gloor, Emanuel -- Higuchi, Niro -- Jimenez, Eliana -- Lloyd, Gareth -- Meir, Patrick -- Mendoza, Casimiro -- Morel, Alexandra -- Neill, David A -- Nepstad, Daniel -- Patino, Sandra -- Penuela, Maria Cristina -- Prieto, Adriana -- Ramirez, Fredy -- Schwarz, Michael -- Silva, Javier -- Silveira, Marcos -- Thomas, Anne Sota -- Steege, Hans Ter -- Stropp, Juliana -- Vasquez, Rodolfo -- Zelazowski, Przemyslaw -- Alvarez Davila, Esteban -- Andelman, Sandy -- Andrade, Ana -- Chao, Kuo-Jung -- Erwin, Terry -- Di Fiore, Anthony -- Honorio C, Euridice -- Keeling, Helen -- Killeen, Tim J -- Laurance, William F -- Pena Cruz, Antonio -- Pitman, Nigel C A -- Nunez Vargas, Percy -- Ramirez-Angulo, Hirma -- Rudas, Agustin -- Salamao, Rafael -- Silva, Natalino -- Terborgh, John -- Torres-Lezama, Armando -- New York, N.Y. -- Science. 2009 Mar 6;323(5919):1344-7. doi: 10.1126/science.1164033.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Ecology and Global Change, School of Geography, University of Leeds, Leeds LS2 9JT, UK. o.phillips@leeds.ac.uk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19265020" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere ; *Biomass ; Brazil ; Carbon ; Carbon Dioxide ; Climate ; *Droughts ; *Ecosystem ; South America ; *Trees/growth & development ; Tropical Climate
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
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    Instituto Oceanográfico de la Armada, Guayaquil, Ecuador
    Publication Date: 2021-05-19
    Description: Usando series de tiempo de promedios diarios de nivel del mar en años caracterizados por la ocurrencia de eventos El Niño en la estación mareográfica de La Libertad (02°15'S-81°27'W), se aplicaron las técnicas del análisis espectral para determinar la correlación existente entre los eventos pasados y el primer semestre de 1997. Se obtuvieron niveles significativos de coherencia entre el evento El Niño 1982-1983 con el evento del 1997. El análisis espectral comparativo permitió obtener las ondas predominantes, la amplitud y el ángulo de fase de cada una de ellas. Con estos parámetros y aplicando la serie de Fourier, se generó una serie del nivel del mar que permitió predecir el comportamiento del nivel del mar en La Libertas desde julio 97 hasta marzo 98 con un 73% de correlación. El método fue óptimo para indicar con buena aproximación el comportamiento dinámico del evento cálido aún cuando los valores absolutos de nivel del mar tuvieron un margen mayor de error. Se evidenció la estrecha relación entre el comportamiento dinámico y térmico del océano durante el desarrollo de un evento El Niño. El análisis de los espectros evidenció el importante aporte de energía de las ondas interestacionales en el océano y sugiere que los eventos El Niño tienen patrones de interacción de las ondas océanicas que podrían ser de naturaleza recurrente y por lo tanto predecibles a partir de datos históricos disponibles.
    Description: Using times series of daily averages of sea level during years of occurrence of events El Niño in the station of La Libertad (02°15'S-81°27'W), techniques of spectral analysis were applied to determine the existence correlation between the last events and the first semester of 1997. Significant levels of coherence were obtained among the event El Niño 1982-1983 with the event of 1997. The comparative spectral analysis allowed to obtain the predominant waves, the amplitude and the angle of phase of each one of them. With this parameters and applying the Fourier series, a sea level serie was generated and allowed to predict the behavior of the sea level in La Libertad since july 1997 until march 1998 with a correlation of 73%. The method was acceptable to indicate with a close approach the dynamic behavior of the warm event when the absolute values of sea level had a bigger margin of error. The narrow relationship was evidenced among the dynamic and thermal behavior of the ocean during the development of an event El Niño. The analysis of the spectra evidenced the important contribution of energy of the intraseasonal waves in the ocean. It suggest that the events El Niño have interaction patterns of the oceanic waves that would be recurred and there fore predictable.
    Description: Incluye ref.bibl., grafs., tbls.
    Description: Published
    Keywords: Prediction ; Spectral analysis ; Sea level ; Prediction ; El Nino phenomena ; Spectral analysis ; Fourier analysis ; Sea level ; Oceanographic data ; Time series
    Repository Name: AquaDocs
    Type: Journal Contribution , Non-Refereed , Article
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  • 3
    Publication Date: 2021-05-19
    Description: El presente trabajo permite conocer el comportamiento de la cuña salina en el sistema Río Guayas - Canal de Jambelí, conociendo que el Río Guayas abastece de agua a Guayaquil, puerto principal del país, y a muchas otras poblaciones.
    Description: The present work allows to establish the behavior of the salinity of the water, time of renovation and its effect on the quality of water in two established stages: increase in the level of the sea in 0.3 m. and 1.0 m. In the System of the Guayas Channel in Jambelí, considering the exchange of waters that exists between the Guayas River and the sea. The horizontal and vertical gradients of salinity are intimately bound with the flow of the Guayas River, as long as the flow increases the intrusion of the saline wedge will be minor. During the dry station the vertical gradients of salinity are maximums in the sector between The Esclusas - Point Stone. It is in this area where they give up the processes of mixture in a higher form. The gradient mentioned changes, being found in the south during the humid season. The gradients of salinity are important in the area already mentioned, after this, the variations don't present too many changes, this is a reason why it can be ignore. The advance of the saline wedge will be harmful, in the cases, where the water is used directly due to that an excess of salted water that will cause damages in the agriculture production of corn, rice, banana tree, etc. as well as the populations settled in the bordes of the Daule and Babahoyo rivers who use the water directly from the river for their daily work.
    Description: Incluye ref.bibl., grafs., tbls.
    Description: Published
    Keywords: Water quality ; Irrigation water ; Rivers ; Sea level ; Water quality ; Sea level ; Climatic changes ; Salt-wedge estuaries ; Salt wedges ; Salinity gradients ; Irrigation water ; River water ; Rivers
    Repository Name: AquaDocs
    Type: Journal Contribution
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  • 4
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    Instituto Oceanográfico de la Armada, Guayaquil, Ecuador
    Publication Date: 2021-05-19
    Description: Se realiza un análisis de las series de tiempo mensuales de los parámetros meteorológicos-oceanográficos y los diferentes flujos de calor obtenidos mediante relaciones empíricas de la estación ubicada en La Libertad desde mediados de 1988 hasta finales de 1997, obteniéndose las climatologías mensuales así como estadísticas interesantes, aparentemente los datos no muestran una relación entre el intercambio de calor superficial y El Niño-Oscilación Sur.
    Description: An analysis is achievied by means of the monthly time series of the parameters meteorological-oceanographic and the different fluxes of heat obtained by empiric relationships of the station located in La Libertad from half-year of 1988 until final of 1997, being obtained the monthly climatologies as well as interesting statistical, seemingly the data don't show a relationship between the exchange of heat surface and El Niño-South Oscillation.
    Description: Incluye ref.bibl., grafs., tbls.
    Description: Published
    Keywords: Climatology ; Time series analysis ; Climatology ; Oceanographic data ; Time series analysis
    Repository Name: AquaDocs
    Type: Journal Contribution
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  • 5
    Publication Date: 2021-05-19
    Description: El objetivo del presente trabajo es estudiar la estructura termohalina superficial y subsuperficial de una región del Pacífico Sudeste (Guayaquil-Valparaíso), Fig. 1, durante el término de la primavera austral de 1997 para determinar los posibles cambios en la circulación. Para esta fecha se dio comienzo la VII Expedición Ecuatoriana a la Antártida a bordo del B/I ORION y simultáneamente se estaba desarrollando un evento ENOS de intensidad fuerte.
    Description: During the VII Ecuadorian Expedition to the Antarctic (December of 1997) the B/I ORION carried out oceanographic stations and XBT launches in the track (Guayaquil-Valparaiso in order to determine the change in circulation and termohaline structure on Southeast Pacific during the development of the ENSO event. By means of Sea Surface Temperature, sections of temperature and salinity diagrams T/S, were observed, positive surface and subsurface anomalies of subtropical surfaces waters that suggest a reforcement of the Equatorial undercurrent those feed the Gunther Undercurrent and the Perú-Chile Countercurrent those go toward the south, forcing to turn early toward the west to the Oceanic Current of Humboldt and to fathom the Chile Coastal Current Measures of direct current even the 100 meters demonstrate the great flow from north.
    Description: Incluye ref.bibl., ilus.
    Description: Published
    Description: Pacifico sudeste
    Keywords: El Nino phenomena ; Thermohaline circulation ; Surface temperature ; T/S diagrams ; Current direction ; Countercurrents ; Current measurement ; Ocean circulation
    Repository Name: AquaDocs
    Type: Journal Contribution , Non-Refereed , Article
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  • 6
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    Instituto Oceanográfico de la Armada, Guayaquil, Ecuador
    Publication Date: 2021-05-19
    Description: El objetivo de este artículo es documentar científicamente la evolución del evento "El Niño" en Ecuador, desde el punto de vista oceanográfico, sugiriendo posibles mecanismos involucrados en este proceso, vinculados a ondas interestacionales Kelvin en el océano (Kessler et al., 1995) que actúan como contraparte a las oscilaciones de 60 a 75 días en la atmósfera (Maden - Julian, 1995) y más específicamente de ondas encontradas en los espectros de nivel medio del mar y TSM en el mar ecuatoriano- colombiano con estas mismas características (Martínez, 1998).
    Description: Incluye ref.bibl., grafs.
    Description: Published
    Keywords: Air temperature ; Variability ; Isotherms ; Thermohaline circulation ; El Nino phenomena ; Surface temperature ; Cruises ; Kelvin waves ; Air temperature ; Mean sea level ; Salinity charts
    Repository Name: AquaDocs
    Type: Journal Contribution , Non-Refereed , Article
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  • 7
    Publication Date: 2022-05-25
    Description: Author Posting. © Elsevier B.V., 2009. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Palaeogeography, Palaeoclimatology, Palaeoecology 294 (2010): 56-71, doi:10.1016/j.palaeo.2009.03.012.
    Description: Since the last deglaciation, the mid-latitudes of the southern Hemisphere have undergone considerable environmental changes. In order to better understand the response of continental ecosystems to paleoclimate changes in southern South America, we investigated the sedimentary record of Puyehue Lake, located in the western piedmont of the Andes in south-central Chile (40°S). We analyzed the elemental (C, N) and stable isotopic (δ13C, δ15N) composition of the sedimentary organic matter preserved in the lake and its watershed to estimate the relative changes in the sources of sedimentary organic carbon through space and time. The geochemical signature of the aquatic and terrestrial end-members was determined on samples of lake particulate organic matter (N/C: 0.130) and Holocene paleosols (N/C: 0.069), respectively. A simple mixing equation based on the N/C ratio of these end-members was then used to estimate the fraction of terrestrial carbon (ƒT) preserved in the lake sediments. Our approach was validated using surface sediment samples, which show a strong relation between ƒT and distance to the main rivers and to the shore. We further applied this equation to an 11.22 m long sediment core to reconstruct paleoenvironmental changes in Puyehue Lake and its watershed during the last 17.9 kyr. Our data provide evidence for a first warming pulse at 17.3 cal kyr BP, which triggered a rapid increase in lake diatom productivity, lagging the start of a similar increase in sea surface temperature (SST) off Chile by 1500 years. This delay is best explained by the presence of a large glacier in the lake watershed, which delayed the response time of the terrestrial proxies and limited the concomitant expansion of the vegetation in the lake watershed (low ƒT). A second warming pulse at 12.8 cal kyr BP is inferred from an increase in lake productivity and a major expansion of the vegetation in the lake watershed, demonstrating that the Puyehue glacier had considerably retreated from the watershed. This second warming pulse is synchronous with a 2°C increase in SST off the coast of Chile, and its timing corresponds to the beginning of the Younger Dryas Chronozone. These results contribute to the mounting evidence that the climate in the mid-latitudes of the southern Hemisphere was warming during the Younger Dryas Chronozone, in agreement with the bipolar see-saw hypothesis.
    Description: This research was partly supported by the Belgian OSTC project EV/12/10B "A continuous Holocene record of ENSO variability in southern Chile". S.B. is supported by a BAEF fellowship (Belgian American Educational Foundation), and by an EU Marie Curie Outgoing Fellowship under the FP6 programme.
    Keywords: Organic matter ; Lake sediments ; Carbon ; Nitrogen ; Southern Hemisphere ; Deglaciation
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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