Oxygen and indicators of stress for marine life in multi-model global warming projections

Decadal-to-century scale trends for a range of marine environmental variables in the upper mesopelagic layer (UML, 100–600 m) are investigated using results from seven Earth System Models forced by a high greenhouse gas emission scenario. The models as a class represent the observation-based distribution of oxygen (O2) and carbon dioxide (CO2), albeit major mismatches between observation-based and simulated values remain for individual models. By year 2100 all models project an increase in SST between 2 °C and 3 °C, and a decrease in the pH and in the saturation state of water with respect to calcium carbonate minerals in the UML. A decrease in the total ocean inventory of dissolved oxygen by 2% to 4% is projected by the range of models. Projected O2 changes in the UML show a complex pattern with both increasing and decreasing trends reflecting the subtle balance of different competing factors such as circulation, production, remineralization, and temperature changes. Projected changes in the total volume of hypoxic and suboxic waters remain relatively small in all models. A widespread increase of CO2 in the UML is projected. The median of the CO2 distribution between 100 and 600m shifts from 0.1–0.2 mol m−3 in year 1990 to 0.2–0.4 mol m−3 in year 2100, primarily as a result of the invasion of anthropogenic carbon from the atmosphere. The co-occurrence of changes in a range of environmental variables indicates the need to further investigate their synergistic impacts on marine ecosystems and Earth System feedbacks.

The past ecology of Abies alba provides new perspectives on future responses of silver fir forests to global warming

Paleoecology can provide valuable insights into the ecology of species that complement observation and experiment-based assessments of climate impact dynamics. New paleoecological records (e.g., pollen, macrofossils) from the Italian Peninsula suggest a much wider climatic niche of the important European tree species Abies alba (silver fir) than observed in its present spatial range. To explore this discrepancy between current and past distribution of the species, we analyzed climatic data (temperature, precipitation, frost, humidity, sunshine) and vegetation-independent paleoclimatic reconstructions (e.g., lake levels, chironomids) and use global coupled carbon-cycle climate (NCAR CSM1.4) and dynamic vegetation (LandClim) modeling. The combined evidence suggests that during the mid-Holocene (6000 years ago), prior to humanization of vegetation, A. alba formed forests under conditions that exceeded the modern (1961-1990) upper temperature limit of the species by 5-7°C (July means). Annual precipitation during this natural period was comparable to today (>700-800 mm), with drier summers and wetter winters. In the meso-Mediterranean to sub-Mediterranean forests A. alba co-occurred with thermophilous taxa such as Quercus ilex, Q. pubescens, Olea europaea, Phillyrea, Arbutus, Cistus, Tilia, Ulmus, Acer, Hedera helix, Ilex aquifolium, Taxus, and Vitis. Results from the last interglacial (ca. 130 000-115 000 BP), when human impact was negligible, corroborate the Holocene evidence. Thermophilous Mediterranean A. alba stands became extinct during the last 5000 years when land-use pressure and specifically excessive anthropogenic fire and browsing disturbance increased. Our results imply that the ecology of this key European tree species is not yet well understood. On the basis of the reconstructed realized climatic niche of the species, we anticipate that the future geographic range of A. alba may not contract regardless of migration success, even if climate should become significantly warmer than today with summer temperatures increasing by up to 5-7°C, as long as precipitation does not fall below 700-800 mm/yr, and anthropogenic disturbance (e.g., fire, browsing) does not become excessive. Our finding contradicts recent studies that projected range contractions under global-warming scenarios, but did not factor how millennia of human impacts reduced the realized climatic niche of A. alba.

Analysis of an ancient global warming event, the Paleocene-Eocene thermal maximum, under examination from ODP Holes 113-689B and 113-690B

Spatiotemporal patterns of carbonate dissolution provide a critical constraint on carbon input during an ancient (~55.5 Ma) global warming event known as the Paleocene-Eocene thermal maximum (PETM), yet the magnitude of lysocline shoaling in the Southern Ocean is poorly constrained due to limited spatial coverage in the circum-Antarctic region. This shortcoming is partially addressed by comparing patterns of carbonate sedimentation at the Site 690 PETM reference section to those herein reconstructed for nearby Site 689. Biochemostratigraphic correlation of the two records reveals that the first ~36 ka of the carbon isotope excursion (CIE) signaling PETM conditions is captured by the Site 689 section, while the remainder of the CIE interval and nearly all of the CIE recovery are missing due to a coring gap. A relatively expanded stratigraphy and higher carbonate content at mid-bathyal Site 689 indicate that dissolution was less severe than at Site 690. Thus, the bathymetric transect delimited by these two PETM records indicates that the lysocline shoaled above Site 689 (~1,100 m) while the calcite compensation depth remained below Site 690 (~1,900 m) in the Weddell Sea region. The ensuing recovery of carbonate sedimentation conforms to a bathymetric trend best explained by gradual lysocline deepening as negative feedback mechanisms neutralized ocean acidification. Further, biochemostratigraphic evidence indicates the tail end of the CIE recovery interval at both sites has been truncated by a hiatus most likely related to vigorous production and advection of intermediate waters.

The early Eocene global warming events: Implications from ODP Leg 208 Walvis Ridge depth transect

Five sections drilled in multiple holes over a depth transect of more than 2200 m at the Walvis Ridge (SE Atlantic) during Ocean Drilling Program (ODP) Leg 208 resulted in the first complete early Paleogene deep-sea record. Here we present high-resolution stratigraphic records spanning a ~4.3 million yearlong interval of the late Paleocene to early Eocene. This interval includes the Paleocene-Eocene thermal maximum (PETM) as well as the Eocene thermal maximum (ETM) 2 event. A detailed chronology was developed with nondestructive X-ray fluorescence (XRF) core scanning records and shipboard color data. These records were used to refine the shipboard-derived spliced composite depth for each site and with a record from ODP Site 1051 were then used to establish a continuous time series over this interval. Extensive spectral analysis reveals that the early Paleogene sedimentary cyclicity is dominated by precession modulated by the short (100 kyr) and long (405 kyr) eccentricity cycles. Counting of precession-related cycles at multiple sites results in revised estimates for the duration of magnetochrons C24r and C25n. Direct comparison between the amplitude modulation of the precession component derived from XRF data and recent models of Earth's orbital eccentricity suggests that the onset of the PETM and ETM2 are related to a 100-kyr eccentricity maximum. Both events are approximately a quarter of a period offset from a maximum in the 405-kyr eccentricity cycle, with the major difference that the PETM is lagging and ETM2 is leading a 405-kyr eccentricity maximum. Absolute age estimates for the PETM, ETM2, and the magnetochron boundaries that are consistent with recalibrated radiometric ages and recent models of Earth's orbital eccentricity cannot be precisely determined at present because of too large uncertainties in these methods. Nevertheless, we provide two possible tuning options, which demonstrate the potential for the development of a cyclostratigraphic framework based on the stable 405-kyr eccentricity cycle for the entire Paleogene.

Rehabilitación energética de fachadas: Propuesta metodológica para la evaluación de soluciones innovadoras, basándose en el diagnóstico de viviendas sociales construidas entre 1940 y 1980

Se propone una metodología para la evaluación de soluciones constructivas de fachada para la rehabilitación de viviendas sociales, construidas entre el final de la Guerra Civil y la entrada en vigor de la norma básica NBE-CT-79, sobre condiciones térmicas en edificios. La metodología parte por un lado del análisis del estado actual en las viviendas, y por otro de la caracterización de las soluciones constructivas de rehabilitación, para la evaluación conjunta de las posibles mejoras. Esta evaluación persigue valorar su repercusión en la calidad del ambiente interior, y en la reducción de la demanda energética para acondicionamiento térmico. Se aplica sobre dos viviendas tipo que se han monitorizado en Madrid, utilizando dos soluciones innovadoras para rehabilitación energética, que disponen de documentos de idoneidad DIT y DITE. Una incorpora sobre la fachada tipo un aislamiento por el exterior, y otra incorpora un sistema de fachada ventilada, también sobre esta fachada tipo. El análisis de las viviendas se ha realizado a partir de la toma de datos, ensayos y estudio de detalle, llevados a cabo a lo largo de los años 2014 y 2015. El análisis de los sistemas de fachada se ha realizado a partir de ensayos controlados, comparando los resultados para tres tipos de fachada: una fachada tipo, habitual en la construcción de las viviendas de este periodo, y las dos soluciones innovadoras mencionadas. Una vez realizado el diagnóstico de las viviendas y el análisis de los ensayos de los sistemas constructivos, los resultados obtenidos se utilizan para generar los modelos de simulación sobre los que evaluar las mejoras. El periodo de estudio comprende cuatro décadas que comienzan en 1940, en un momento con escasos medios técnicos para la construcción, y que coincide con el comienzo del crecimiento en las grandes ciudades, y finaliza con la incorporación en la normativa de las exigencias de aislamiento en fachadas, de 1979. En la ciudad de Madrid las viviendas construidas en este periodo, suponen un 45% del total de viviendas censadas en 2011. La rehabilitación energética se ha ido incorporando en los sucesivos planes nacionales de vivienda como actuación protegida, y son muchos y muy diversos los planes de acción desde la administración en materia de vivienda social, tanto a nivel nacional como europeo. La vivienda queda incluida en materia de desarrollo y cohesión urbana, territorial y social, haciendo necesario un enfoque integrado. Los barrios de vivienda social forman parte de un patrimonio construido en los que los criterios de sostenibilidad toman especial interés y relevancia, ya que a través del tiempo se han construido como actores y testigos de su historia social, económica, ambiental y cultural. El diseño de los modelos y actuaciones de futuro se sustenta en la asimilación de esa complejidad y diversidad adquirida. Por otro lado, el actual reto que impone el calentamiento global obliga a plantear escenarios de adaptación y mejora en estos edificios, con una especial atención a la dependencia energética, el consumo de recursos, y emisiones de gases de efecto invernadero. La fachada es el elemento más importante de la envolvente en los edificios multifamiliares, siendo el lugar donde se produce el intercambio entre el ambiente interior y exterior. Su rehabilitación puede mejorar las prestaciones de habitabilidad en las viviendas, y disminuir la demanda de energía para alcanzar unas condiciones de confort estándar. El trabajo de investigación que se ha realizado, forma parte de una linea de investigación abierta sobre sistemas constructivos y habitabilidad en edificación. ABSTRACT A methodology for the evaluation of facade’s constructive solutions for social housing refurbishment, built between the end of the Civil War, and the entry into force of the basic standard NBE-CT-79 on thermal conditions in buildings is proposed. This methodology starts both with the analysis of the current status in dwellings, and with the characterization of rehabilitation’s constructive solutions performance, for the integrated assessment of improvements. The evaluation seeks to assess their impact on the indoor environmental quality, and on reducing the energy demand for thermal conditioning. The methodology is applied to two standard dwellings, that have been monitored in Madrid, with two innovative solutions for energy refurbishment, which have DIT and DITE assessment documents. One incorporates an exterior insulation, and the other incorporates a ventilated facade system. The analysis of the dwellings was made from data collection, testing and detailed study, conducted throughout 2014 and 2015. Analysis of the facade systems was made from controlled trials comparing the results for three types of façade: a standard usual facade common in the construction of this period, and the two innovative solutions mentioned. Based on the diagnosis of housing and systems analysis, the results are used to generate simulation models on which assess the improvements. The study period comprises four decades starting in 1940, at a time with limited technical resources for construction, which coincides with the beginning of growth in big cities, and ends with the incorporation in the 1979 legislation of the façade’s insulation requirements. In the city of Madrid the houses built in this period account for 45% of all households surveyed in 2011. As a “protected action” energy rehabilitation has been incorporated in successive national housing plans, and there are many and very different action plans from the Administration in the field of social housing, both at national and European level. An integrated approach is needed, due to the inclusion of housing in development and urban, territorial and social cohesion. Social housing neighborhoods are part of the built heritage. Sustainability criteria therefore are particularely relevant, since over time they have been built as actors and witnesses of their social, economic, environmental and cultural history. The design and performance of future models is based on the assimilation of this complexity and diversity acquired. On the other hand, the current challenge posed by global warming forces to consider scenarios for adaptation and improvement in these buildings, with particular attention to energy dependence, resource consumption, and greenhouse gas emissions. The facade is the most important element of the envelope in the multi-family buildings, being the place where the exchange occurs between the indoor and outdoor environments. Its rehabilitation can improve wellbeing in housing performance, and reduce energy demand to achieve standard comfort conditions. This research that has been done, is part of an open research line on construction and living conditions in buildings.

The Contribution of Agriculture, Forestry and other Land Use activities to Global Warming, 1990-2012

Date of Acceptance: 16/12/2014 Acknowledgements: This work was carried out with generous funding by the Governments of Germany (GCP/GLO/286/GER) and Norway (GCP/GLO/325/NOR) to the ‘Monitoring and Assessment of GHG Emissions and Mitigation Potential from Agriculture’ Project of the FAO Climate, Energy and Tenure Division. P. Smith is a Royal Society Wolfson Merit Award holder, and his input contributes to the University of Aberdeen Environment and Food Security Theme and to Scotland's ClimateXChange. J. House was funded by a Leverhulme Research Fellowship. The FAO Statistics Division maintains the FAOSTAT Emissions database with regular program funds allocated through Strategic Objective 6. © 2015 John Wiley & Sons Ltd.

Global warming in the twenty-first century: An alternative scenario

A common view is that the current global warming rate will continue or accelerate. But we argue that rapid warming in recent decades has been driven mainly by non-CO2 greenhouse gases (GHGs), such as chlorofluorocarbons, CH4, and N2O, not by the products of fossil fuel burning, CO2 and aerosols, the positive and negative climate forcings of which are partially offsetting. The growth rate of non-CO2 GHGs has declined in the past decade. If sources of CH4 and O3 precursors were reduced in the future, the change in climate forcing by non-CO2 GHGs in the next 50 years could be near zero. Combined with a reduction of black carbon emissions and plausible success in slowing CO2 emissions, this reduction of non-CO2 GHGs could lead to a decline in the rate of global warming, reducing the danger of dramatic climate change. Such a focus on air pollution has practical benefits that unite the interests of developed and developing countries. However, assessment of ongoing and future climate change requires composition-specific long-term global monitoring of aerosol properties.

The observed global warming record: What does it tell us?

Global, near-surface temperature data sets and their derivations are discussed, and differences between the Jones and Intergovernmental Panel on Climate Change data sets are explained. Global-mean temperature changes are then interpreted in terms of anthropogenic forcing influences and natural variability. The inclusion of aerosol forcing improves the fit between modeled and observed changes but does not improve the agreement between the implied climate sensitivity value and the standard model-based range of 1.5–4.5°C equilibrium warming for a CO2 doubling. The implied sensitivity goes from below the model-based range of estimates to substantially above this range. The addition of a solar forcing effect further improves the fit and brings the best-fit sensitivity into the middle of the model-based range. Consistency is further improved when internally generated changes are considered. This consistency, however, hides many uncertainties that surround observed data/model comparisons. These uncertainties make it impossible currently to use observed global-scale temperature changes to narrow the uncertainty range in the climate sensitivity below that estimated directly from climate models.

Technologies for remediating global warming [microform] : hearing before the Subcommittee on Natural Resources, Agriculture Research and Environment and the Subcommittee on Science, Research and Technology of the Committee on Science, Space, and Technology, U.S. House of Representatives, One Hundredth Congress, second session, June 29, 1988

Distributed to some depository libraries in microfiche. "No. 137."