Climate Change and Global Wine Quality   总被引：10，自引：0，他引：10  

Gregory?V.?JonesEmail author  Michael?A.?White  Owen?R.?Cooper  Karl?Storchmann 《Climatic change》2005,73(3):319-343

From 1950 to 1999 the majority of the world's highest quality wine-producing regions experienced growing season warming trends. Vintage quality ratings during this same time period increased significantly while year-to-year variation declined. While improved winemaking knowledge and husbandry practices contributed to the better vintages it was shown that climate had, and will likely always have, a significant role in quality variations. This study revealed that the impacts of climate change are not likely to be uniform across all varieties and regions. Currently, many European regions appear to be at or near their optimum growing season temperatures, while the relationships are less defined in the New World viticulture regions. For future climates, model output for global wine producing regions predicts an average warming of 2 ^∘C in the next 50 yr. For regions producing high-quality grapes at the margins of their climatic limits, these results suggest that future climate change will exceed a climatic threshold such that the ripening of balanced fruit required for existing varieties and wine styles will become progressively more difficult. In other regions, historical and predicted climate changes could push some regions into more optimal climatic regimes for the production of current varietals. In addition, the warmer conditions could lead to more poleward locations potentially becoming more conducive to grape growing and wine production.  相似文献   

Petrology and petrogenesis of carbonatitic rocks in syenites from central Anatolia,Turkey     

Alan F. Cooper  Durmus Boztuğ  J. Michael Palin  Candace E. Martin  Mihoko Numata 《Contributions to Mineralogy and Petrology》2011,161(5):811-828

The late Cretaceous A-type Karaçay?r pluton in Central Anatolia, Turkey, intrudes and entrains xenoliths of Palaeozoic limestone. Carbonatitic magmatic rocks within the syenite have been previously interpreted (Schuiling in Nature, 192:1280, 1961) to result from metasomatic alteration and syntectic melting of marble. Carbonatites and associated calcite-syenites exhibit mineralogical characteristics (Ab-rich plagioclase, Ba-rich K-feldspar, low-Mg# biotite) that are petrogenetically more evolved than the host syenitic suite. Geochemically, carbonate-rich magmatic rocks are greatly enriched in Sr, Ba, Th, and REE and have higher LREE/HREE ratios than either syenites or marbles. In terms of O-C-Sr-Pb isotope ratios, the carbonatite/calcite-syenite suite form a consistent and geochemically coherent group that is distinct from the marble country rock and xenolith population, but similar to some of the syenitic, and particularly the nepheline syenite components of the Karaçay?r pluton. Other silicate magmatic rocks are geochemically, isotopically, and geochronologically different, suggesting the pluton is composite. Overall, the mineralogical and geochemical characteristics of the carbonatites are incompatible with binary mixing of syenite and marble but are consistent with derivation of carbonatite from petrogenetically evolved foid syenite. Carbonate–silicate rock types have modal variations compatible with an origin by fractional crystallisation, rather than by liquid immiscibility.  相似文献   

Investigation of three‐dimensional wind flow behaviour over coastal dune morphology under offshore winds using computational fluid dynamics (CFD) and ultrasonic anemometry     

D. W. T. Jackson  J. H. M. Beyers  K. Lynch  J. A. G. Cooper  A. C. W. Baas  I. Delgado‐Fernandez I 《地球表面变化过程与地形》2011,36(8):1113-1124

The behaviour of offshore‐directed winds over coastal dune and beach morphology was examined using a combination of modelling (3‐D computational fluid dynamics (CFD)) and field measurement. Both model simulations and field measurements showed reversal of offshore flows at the back beach and creation of an onshore sediment transport potential. The influence of flow reversals on the beach‐dune transport system and foredune growth patterns has previously received little attention. Detailed wind flow measurements were made using an extensive array of mast‐mounted, 3‐D ultrasonic anemometers (50 Hz), arranged parallel to the dominant incident wind direction. Large eddy simulation (LES) of the offshore wind flow over the dune was conducted using the open‐source CFD tool openFOAM. The computational domain included a terrain model obtained by airborne LiDAR and detailed ground DGPS measurements. The computational grid (~22 million cells) included localized mesh refinement near the complex foredune terrain to capture finer details of the dune morphology that might affect wind flows on the adjacent beach. Measured and simulated wind flow are presented and discussed. The CFD simulations offer new insights into the flow mechanics associated with offshore winds and how the terrain steering of wind flow impacts on the geomorphological behaviour of the dune system. Simulation of 3‐D wind flows over complex terrain such as dune systems, presents a valuable new tool for geomorphological research, as it enables new insights into the relationship between the wind field and the underlying topography. The results show that offshore and obliquely offshore winds result in flow reversal and onshore directed winds at distances of up to 20 m from the embryo dune toe. The potential geomorphological significance of the findings are discussed and simple calculations show that incoming offshore and obliquely offshore winds with mean velocities over 13 m s^?1 and 7 m s^?1, respectively, have the potential to create onshore‐directed winds at the back beach with mean velocities above 3.3 m s^?1. These are above the threshold of movement for dry sand and support previous conclusions about the significance of offshore winds in dune and beach budget calculations. Copyright © 2011 John Wiley & Sons, Ltd.  相似文献   

Progress in Integrated Coastal Zone Management (ICZM) in Northern Ireland     

J.A.G. Cooper 《Marine Policy》2011

The history of development of Integrated Coastal Zone Management (ICZM) in Northern Ireland is described here in the context of European and UK initiatives. The current structures for ICZM in Northern Ireland involve a formal strategy. This involves a number of specific actions in the environmental, social, and economic spheres with specific goals pertaining to integration. The strategy has been agreed by all responsible organisations (both governmental and NGOs), and each action is time-bound and has an identified responsible agency. The Northern Ireland Coastal and Marine Forum (NICMF) which consists of non-governmental members, has the task of monitoring the implementation of the strategy and acting as a catalyst for integration. The strengths of the current structure lie in the presence of an integrating ICZM strategy and the fact that the initiative is government-led in response to the EU Recommendation on ICZM. These provide better levels of sustainability and links to the statutory system of governance compared to the partnership model in Great Britain. Its main weaknesses are: (i) that the NICMF relies on voluntary participation; (ii) linkages between government departments have not been substantially improved; and (iii) weak mechanisms for ensuring goals are achieved.  相似文献   

A tree-ring reconstruction of East Anglian (UK) hydroclimate variability over the last millennium     

Richard J. Cooper  Thomas M. Melvin  Ian Tyers  Rob J. S. Wilson  Keith R. Briffa 《Climate Dynamics》2013,40(3-4):1019-1039

We present an annually resolved reconstruction of spring-summer precipitation variability in East Anglia, UK (52–53°N, 0–2°E) for the period AD 900–2009. A continuous regional network of 723 living (AD 1590–2009) and historical (AD 781–1790) oak (Quercus sp.) ring-width series has been constructed and shown to display significant sensitivity to precipitation variability during the March-July season. The existence of a coherent common growth signal is demonstrated in oaks growing across East Anglia, containing evidence of near-decadal aperiodic variability in precipitation throughout the last millennium. Positive correlations are established between oak growth and precipitation variability across a large region of northwest Europe, although climate-growth relationships appear time transgressive with correlations significantly weakening during the early twentieth century. Examination of the relationship between oak growth, precipitation, and the North Atlantic Oscillation (NAO), reveals no evidence that the NAO plays any significant role in the control of precipitation or tree growth in this region. Using Regional Curve Standardisation to preserve evidence of low-frequency growth variability in the East Anglian oak chronology, we produce a millennial length reconstruction that is capable of explaining 32–35% of annual-to-decadal regional-scale precipitation variance during 1901–2009. The full length reconstruction indicates statistically significant anomalous dry conditions during AD 900–1100 and circa-1800. An apparent prolonged wetter phase is estimated for the twelfth and thirteen centuries, whilst precipitation fluctuates between wetter and drier phases at near centennial timescales throughout the fourteenth to seventeenth centuries. Above average precipitation reconstructed for the twenty-first century is comparable with that reproduced for the 1600s. The main estimated wet and dry phases reconstructed here appear largely coherent with an independent tree-ring reconstruction for southern-central England.  相似文献   

Experimental study of water fluxes in a residential area: 1. Rainfall,roof runoff and evaporation: the effect of slope and aspect     

R. Ragab  J. Bromley  P. Rosier  J. D. Cooper  J. H. C. Gash 《水文研究》2003,17(12):2409-2422

An experimental study of water fluxes from roofs in a residential area has quantified water fluxes from different types of roof and identified the major controls on the process. Roofs with pitches of 0°, 22° and 50° and orientations of 15° (from true north) (NNE) and 103° (ESE) were selected. A novel automatic system for monitoring has been developed. Noticeable differences in rainfall, runoff and evaporation were found for different roof slopes, aspects and heights. Depending on height, flat roofs collected 90 to 99% of rainfall recorded at ground level. Roofs with a 22° slope; facing south‐south‐west (i.e. facing the prevailing wind) captured most rain, whereas east‐south‐east facing roofs with slopes of 50° received the least. Depending on the roof slope, the average rainfall captured ranged from 62 to 93% of that at ground level. For the same slope, the results indicated that from roofs orientated normal to the prevailing wind; (i) captured rainfall was higher, (ii) evaporation was higher and (iii) runoff was less than that from roofs having other aspects. Monthly variations in the runoff–rainfall ratio followed the rainfall distribution, being lowest in summer and highest in winter. The highest mean ratio (0·91) was associated with the steeper roof slope; the lowest ratio (0·61) was for roofs facing the prevailing wind direction. For the same amount of rainfall, the runoff generated from a steeper roof was significantly higher than that generated by a moderate roof slope, but the lowest runoff was from roofs facing the prevailing wind. The results have also shown that the amount of runoff collected (under UK climatic condition) was sufficient to supply an average household in the studied area with the major part of its annual water requirements. The use of this water not only represents a financial gain for house owners but also will help protect the environment by reducing demand on water resources through the reduction of groundwater abstraction, construction of new reservoirs, and a reduction of the flood risk as its in situ use is considered a preventive measure known as a source control. Copyright © 2003 John Wiley & Sons, Ltd.  相似文献   

Silicon-on-Insulator-Based Single-Chip Image Sensors: Low-Voltage Scientific Imaging     

Vyshnavi Suntharalingam  Barry E. Burke  Michael J. Cooper 《Experimental Astronomy》2002,14(2):91-98

A low-voltage (≤3.3 V) imaging technology has been developed to enable scientific-grade imagers with low-power complex functions on chip. A 128 × 128 CCD imager with on-chip clocking and charge-domain analog-to-digital conversion, as well as an exploratory active pixel sensor have been demonstrated. A 640 × 960 CCD imager with optimized 12 bit charge-domain conversion and an improved active pixel sensor are presently in fabrication. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

Redating the advance of the New Zealand Franz Josef Glacier during the Last Termination: evidence for asynchronous climate change     

C.S.M. Turney  R.G. Roberts  N. de Jonge  C. Prior  J.M. Wilmshurst  M.S. McGlone  J. Cooper 《Quaternary Science Reviews》2007,26(25-28):3037-3042

Dating climatic and environmental records with accuracy and precision is critical if we are to robustly test hypotheses of synchronous change between the hemispheres. In the southern hemisphere, the advance of the New Zealand Franz Josef Glacier to the Waiho Loop terminal moraine has been used as evidence of synchronous global change during the Younger Dryas Chronozone. However, radiocarbon ages for wood incorporated into the sediments associated with the advance span an interval of 900 years. Here we demonstrate that weathered ‘old’ wood was incorporated into the deposit prior to, or during, the advance, and that this material is highly susceptible to contamination by young carbon, resulting in the wide range of age estimates reported previously. We have identified material with little evidence of reworking (well-preserved wood with bark attached) that provides a statistically robust mean radiocarbon age of 11,062±30 BP (13.1 ka) for the advance of the Franz Josef Glacier. The timing of this event falls within the later part of the Antarctic Cold Reversal. Comparison with local, regional and global records suggests that cold conditions in the Southern Ocean were probably experienced in New Zealand at this time, driving the glacial advance.  相似文献   

Combining the use of gradients and reference areas to study bioaccumulation in wild oysters in the Hunter River estuary, New South Wales, Australia     

Lincoln-Smith MP  Cooper TF 《Marine pollution bulletin》2004,48(9-10):873-883

Two approaches for measuring the effects of human activities on aquatic biota are gradient studies and comparison of impacted areas to external references. Wild oysters were sampled at 12 sites adjacent to, upstream and downstream of a steelworks in the Hunter River estuary and in two reference estuaries. Regression analyses for the Hunter indicated reduced concentrations with distance from the point source for some metals and PAHs. Data compared from the reference estuaries to the two sites nearest and the two furthest from the point source in the Hunter indicated elevated concentrations of contaminants both near the point source and on an estuary-wide basis. The gradient approach was useful in identifying the industrial effluent as a point source for bioavailable chemicals. Combining this with the use of reference estuaries provided a broad geographic context in which to interpret results from the Hunter and identified estuary-wide effects.  相似文献   

Probing the Fundamental Physics of the Solar Corona with Lunar Solar Occultation Observations     

S. Rifai Habbal  H. Morgan  M. Druckmüller  A. Ding  J. F. Cooper  A. Daw  E. C. Sittler Jr. 《Solar physics》2013,285(1-2):9-24

Imaging and spectroscopy of the solar corona, coupled with polarimetry, are the only tools available at present to capture signatures of physical processes responsible for coronal heating and solar wind acceleration within the first few solar radii above the solar limb. With the recent advent of improved detector technology and image processing techniques, broad-band white light and narrow-band multi-wavelength observations of coronal forbidden lines, made during total solar eclipses, have started to yield new views about the thermodynamic and magnetic properties of coronal structures. This paper outlines these unique capabilities, which until present, have been feasible primarily with observations during natural total solar eclipses. This work also draws attention to the exciting possibility of greatly increasing the frequency and duration of solar eclipse observations with Moon orbiting observatories utilizing lunar limb occultation of the solar disk for coronal measurements.  相似文献