Home About us Contact
|
Home About us Contact | ||
|
|
||
Northern Regions (northern + regions)
Selected AbstractsGlobalization vs. localization: global food challenges and local solutionsINTERNATIONAL JOURNAL OF CONSUMER STUDIES, Issue 3 2010Quaye Wilhelmina Abstract The objective of this study was to examine the effect of global,local interactions on food production and consumption in Ghana, and identify possible local solutions. Primary data were collected using a combination of quantitative-qualitative methods, which included focus group discussions and one-on-one interviews. Approximately 450 household heads were randomly selected and interviewed between August 2007 and August 2008 in Eastern, Central, Upper East and Northern Regions of Ghana. Findings revealed increasing consumption of foreign rice as opposed to decreasing consumption of local rice and other staples like millet, sorghum and yam because of global,local interactions. However, opportunities exist to re-localize production-consumption patterns through the use of ,glocal foods' like improved ,koose and waakye'. Referencing the situation in Ghana, the study recommends improved production and processing practices backed with appropriate technologies that reflect changing consumption dynamics in order to take full advantage of opportunities created as a result of global,local interactions. [source] Geographic variations in outcome of very low birth weight infants in ItalyACTA PAEDIATRICA, Issue 1 2007Carlo Corchia Abstract Aim: A number of social and health aspects in Italy show remarkable geographic dishomogeneity. We investigated if this phenomenon involves the outcome of very low birth-weight infants (VLBWI). Methods: This is a multi-centre nation-based survey among all Italian NICUs. The number of VLBWI admitted to each NICU in 2001 by birth-weight classes of 250 g, their inborn/outborn status and survival at discharge were registered through ad hoc questionnaires. The data were analysed for the whole country and for three geographic areas (North, Centre and South). Results: A total of 4679 VLBWI in 125 units were surveyed (0.88% of live births in Italy in 2001). The median number of infants admitted was 34 per NICU (interquartile range 16,52), without significant differences among the three geographic areas. The inborn rate was 80.7% (86.5% in the North, 83.7% in the Centre and 74.6% in the South). The mortality rate was 19.6% (15.6% in the North, 19.3% in the Centre and 23.4% in the South). Adjusted relative risk of death between Southern and Northern regions was 1.48 (95% CI 1.30,1.68), and that between outborn and inborn infants was 1.20 (95% CI 1.04,1.37). Conclusions: The differences in mortality among geographic areas suggest a state of socio-sanitary deprivation in the Southern regions, as well as different models of organisation and quality of perinatal care. [source] An experimental evaluation of ice cover effects on the dynamic behaviour of a concrete gravity damEARTHQUAKE ENGINEERING AND STRUCTURAL DYNAMICS, Issue 12 2002Patrick Paultre Abstract An extensive forced-vibration testing programme has been carried out on an 84-m concrete gravity dam located in northeastern Québec, Canada. The dam was subjected to a harmonic load on the crest in summer and severe winter conditions with temperatures ranging from ,10°C to ,15°C and a 1.0,1.5m ice cover. Acceleration and hydrodynamic frequency responses were obtained in different locations on the dam and in the reservoir. The main objective of the repeated tests was to investigate the effects of the ice cover on the dynamic behaviour of the dam,reservoir,foundation system, by comparing summer and winter results. Modifications in damping and resonance frequencies were observed, as well as an additional resonance that was attributed to an interaction of the dam with the ice cover. These findings provided a reliable and unique database for the investigations of dam,reservoir,foundation interaction and, in particular, the ice-cover effects for dams located in northern regions. Copyright © 2002 John Wiley & Sons, Ltd. [source] Temporal and spatial responses of British Columbia steelhead (Oncorhynchus mykiss) populations to ocean climate shiftsFISHERIES OCEANOGRAPHY, Issue 1 2000Welch The pattern of temporal change in recruitment of steelhead trout (Oncorhynchus mykiss) entering the ocean between 1963 and 1990 was geographically coherent in all regions of British Columbia. A major increase in recruitment was evident for smolts entering the ocean after 1977. Subsequently, an out-of-phase response occurred after 1990, indicating that the effect of a possible 1990 regime shift had both temporal and geographical structure. Steelhead entering northern regions had increasing recruitment, while steelhead entering southern BC coastal regions had sharply decreasing recruitment. The evidence clearly indicates that the overall recruitment response since 1977 was primarily shaped by changes in marine (not freshwater) survival. Similar sudden changes in adult recruitment also appear to be occurring for other species of Pacific salmon in BC and Oregon, such as coho (O. kisutch), which appear to occur suddenly and show considerable persistence. A possible explanation for the change is that ocean productivity declined in coastal regions of southern BC after 1990, reducing the marine growth of juvenile salmon. The Bakun upwelling index shows a pattern of geographical coherence along the west coast of North America that could in principle explain the observed pattern of changes in recruitment. However, no evidence for a temporal shift in this index occurring around 1977 and 1990 is apparent. The reason for the sudden and persistent decline in ocean survival is therefore uncertain. [source] Influence of seasonal pressure patterns on temporal variability of vegetation activity in Central SiberiaINTERNATIONAL JOURNAL OF CLIMATOLOGY, Issue 3 2006Sergio M. Vicente-Serrano Abstract This paper analyses the spatial distribution of the inter-annual variability of vegetation activity in central Siberia and its relationship with atmospheric circulation variability. We used NOAA-AVHRR NDVI series from Pathfinder Land Data Set at 1° of spatial resolution, and we calculated the annual vegetation activity in each pixel (aNDVI) from 1982 to 2001. Principal component analysis (PCA) was used to determine the general spatial patterns of inter-annual variability of vegetation activity. We identified three main modes, which explain more than 50% of the total variance, each corresponding to a large region. By means of surface pressure grids, we analysed the main patterns of the seasonal atmospheric circulation in the study area: its variability was summarised by means of a few circulation modes and the patterns differ significantly between winter, spring and summer. However, a pattern with a North,South dipole structure represents the general spatial pattern of atmospheric circulation. We investigated the effect of seasonal atmospheric circulation patterns on the inter-annual variation of vegetation activity. In general, the strongest relationships between the atmospheric circulation variability, climate and the aNDVI variability were found in areas where the climatic characteristics are more limiting for the vegetation development, such as the northern regions. This may be explained by the fact that in these areas the variability of atmospheric circulation modes determines summer temperatures, which have a direct impact on vegetation activity. Copyright © 2006 Royal Meteorological Society. [source] Spatial distribution and its seasonality of satellite-derived vegetation index (NDVI) and climate in SiberiaINTERNATIONAL JOURNAL OF CLIMATOLOGY, Issue 11 2001Rikie Suzuki Abstract The Normalized Difference Vegetation Index (NDVI) distribution and its seasonal cycle were investigated in relation to temperature and precipitation over Siberia and its surrounding regions. The analyses used 5-year (1987,1991) monthly means. The monthly mean NDVI was calculated from the third-generation monthly Global Vegetation Index (GVI) product; monthly temperature and precipitation at 611 stations were calculated from Global Daily Summary (GDS) data. The 611 stations were classified by cluster analysis into 10 classes based on the NDVI seasonal cycle (March,October). The geographical distribution characteristics of the NDVI cycle were described using temperature, precipitation and Olson's land-cover type. In northern regions, where tundra vegetation prevails and temperatures and precipitation are low, the amplitude of the NDVI seasonal cycle is small. In southern regions, where temperatures are high and there is little precipitation, the seasonal amplitude of the NDVI is small because of the arid land type. Forested regions were split into six classes, each characterized by large amplitudes in the NDVI seasonal cycle. The phenological characteristics of the forest classes were noted. For example, a forest-class localized near Lake Baikal shows higher NDVI values, even with the presence of snow cover in March, compared with other regions. This high NDVI value suggests that the exposed green canopy of the coniferous forest can be observed even when snow is present. In addition, the NDVI peaks at stations near 60°N, where the maximum monthly temperature is around 18°C. This result suggests that the optimum temperature-precipitation environment coincides to the area in Siberia where the maximum monthly temperature is 18°C. Copyright © 2001 Royal Meteorological Society [source] Precipitation and atmospheric circulation patterns at mid-latitudes of AsiaINTERNATIONAL JOURNAL OF CLIMATOLOGY, Issue 5 2001Elena M. Aizen Abstract Analyses of the coupling between large-scale atmospheric patterns and modifications of regional precipitation regimes at seasonal and annual time scales in different terrain of mid-latitudes in Asia, including western Siberia, Tien Shan and Pamir mountains, and plains of middle Asia and Japanese Islands, were examined based on data from 57 and 88 hydro-climatic stations with 100 and 60 year records, respectively. For the past 100 years, a positive trend in precipitation was revealed in western Siberia, northern regions of Tien Shan and Japanese Islands. North Atlantic Oscillation (NAO) and West Pacific Oscillation (WPO) indices have inverse associations, with average amount of precipitation in western Siberia and in mountains and plains of middle Asia, and positive correlation in central and western regions of Japanese Islands. The Pacific North American (PNA) index is positively correlated with annual precipitation over most of the Japanese Islands. Northern Asian (NA) positive anomalies lead to decrease in winter precipitation in the western and eastern regions of Japanese Islands. We did not find significant impact of PNA or NA on precipitation in middle Asia. We suggest that during the last century, impacts of the western jet stream increased in the northern regions of Tien Shan and Japanese Islands, and weakened in the eastern Japanese Islands. There is a suggestion that conditions are more favourable for precipitation development over continental regions of Asia when the Siberian High is positioned further to the east than further to the west. During dominant development of a zonal atmospheric pattern, the annual and seasonal precipitation decreased over most regions in continental Asia and central Japan. Copyright © 2001 Royal Meteorological Society [source] A multicentury perspective on the summer North Atlantic Oscillation (SNAO) and drought in the eastern Atlantic Region,JOURNAL OF QUATERNARY SCIENCE, Issue 5 2009Hans W. Linderholm Abstract The summer North Atlantic Oscillation (SNAO) is strongly associated with July,August climate variability over Europe, especially in northern regions. This association includes drought, where a positive SNAO corresponds to dry conditions over much of northern Europe and wet conditions in southern Europe, but the SNAO/climate association is weaker and less homogeneous in the south. Here we use a dendroclimatological reconstruction of the SNAO for the last 550 a to investigate the SNAO/drought relationship in the past. An association between the SNAO and a regional summer drought index from Sweden suggests that the northern European drought relationship holds back to 1700. In the last 550 a, the relationship between SNAO and drought in the Mediterranean region as a whole is weak, but over the Eastern Mediterranean the relationship is clearer and statistically significant (P,<,0.05 level). The Mediterranean relationship is clearest at century scales. An association between the SNAO and Sahel rainfall can clearly be seen on interannual as well as longer timescales in the 20th century. Past droughts in the Sahel, as inferred from historical data, correspond quite well with positive phases of the SNAO on multidecadal timescales back to 1500, the phase expected from instrumental data. The physical reasons for the relationship between Sahel rainfall and the SNAO are, however, not yet understood. This research is a first step towards understanding how the atmospheric circulation over the North Atlantic region affects drought, necessary for forecast future droughts. Copyright © 2009 John Wiley & Sons, Ltd. and © Crown Copyright 2009. [source] MODELED REGIONAL CLIMATE CHANGE IN THE HYDROLOGIC REGIONS OF CALIFORNIA: A CO2 SENSITIVITY STUDY,JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, Issue 3 2004Mark A. Snyder ABSTRACT: Using a regional climate model (RegCM2.5), the potential impacts on the climate of California of increasing atmospheric CO2 concentrations were explored from the perspective of the state's 10 hydrologic regions. Relative to preindustrial CO2 conditions (280 ppm), doubled preindustrial CO2 conditions (560 ppm) produced increased temperatures of up to 4°C on an annual average basis and of up to 5°C on a monthly basis. Temperature increases were greatest in the central and northern regions. On a monthly basis, the temperature response was greatest in February, March, and May for nearly all regions. Snow accumulation was significantly decreased in all months and regions, with the greatest reduction occurring in the Sacramento River region. Precipitation results indicate drier winters for all regions, with a large reduction in precipitation from December to April and a smaller decrease from May to November. The result is a wet season that is slightly reduced in length. Findings suggest that the total amount of water in the state will decrease, water needs will increase, and the timing of water availability will be greatly perturbed. [source] Phylogenetic relationships and pathogenicity of Colletotrichum acutatum isolates from grape in subtropical AustraliaPLANT PATHOLOGY, Issue 3 2007M. A. Whitelaw-Weckert The identity of Colletotrichum acutatum as the causal pathogen of grape ripe-rot, which causes yield loss and a bitter taint that lowers wine quality in Australian subtropical wine-grape regions, was confirmed using species-specific primers. Cultural, morphological and molecular methods (RAPD-PCR and sequencing of parts of the 5·8S-ITS regions and the ,-tubulin-2 gene) were used to determine the phylogenetic relationships of Australian C. acutatum isolates from wine grapes and other horticultural crops. A combination of RAPD-PCR and ,-tubulin-2 gene data showed that all wine-grape ripe-rot isolates from northern regions of New South Wales (NSW) and Queensland belong to a proposed new C. acutatum group (A9), together with isolates from Australian strawberry, mango, blueberry and olive. The 5·8S-ITS sequences for these grape pathogens were identical to published sequences for an isolate from Cyclamen (the Netherlands) and differed by 1 bp from isolates from Capsicum (Taiwan) and orange (Costa Rica). The grape ripe-rot isolates from the Shoalhaven Valley (southern NSW) were clustered within two other C. acutatum groups: A2 and A5. In vitro infection studies showed that Australian C. acutatum isolates from almond, blueberry, chilli, grape, mango, olive, strawberry and tomato were able to infect grape and could also infect blueberry and strawberry, indicating a lack of host specificity. This lack of host specificity, the genetic similarity with non-grape isolates, and the fact that many of the non-grape hosts were isolated from wine-growing regions, suggest the potential for cross-infection between grape and other horticultural crops. [source] Climate change and freshwater biodiversity: detected patterns, future trends and adaptations in northern regionsBIOLOGICAL REVIEWS, Issue 1 2009Jani Heino Abstract Current rates of climate change are unprecedented, and biological responses to these changes have also been rapid at the levels of ecosystems, communities, and species. Most research on climate change effects on biodiversity has concentrated on the terrestrial realm, and considerable changes in terrestrial biodiversity and species' distributions have already been detected in response to climate change. The studies that have considered organisms in the freshwater realm have also shown that freshwater biodiversity is highly vulnerable to climate change, with extinction rates and extirpations of freshwater species matching or exceeding those suggested for better-known terrestrial taxa. There is some evidence that freshwater species have exhibited range shifts in response to climate change in the last millennia, centuries, and decades. However, the effects are typically species-specific, with cold-water organisms being generally negatively affected and warm-water organisms positively affected. However, detected range shifts are based on findings from a relatively low number of taxonomic groups, samples from few freshwater ecosystems, and few regions. The lack of a wider knowledge hinders predictions of the responses of much of freshwater biodiversity to climate change and other major anthropogenic stressors. Due to the lack of detailed distributional information for most freshwater taxonomic groups and the absence of distribution-climate models, future studies should aim at furthering our knowledge about these aspects of the ecology of freshwater organisms. Such information is not only important with regard to the basic ecological issue of predicting the responses of freshwater species to climate variables, but also when assessing the applied issue of the capacity of protected areas to accommodate future changes in the distributions of freshwater species. This is a huge challenge, because most current protected areas have not been delineated based on the requirements of freshwater organisms. Thus, the requirements of freshwater organisms should be taken into account in the future delineation of protected areas and in the estimation of the degree to which protected areas accommodate freshwater biodiversity in the changing climate and associated environmental changes. [source] | ||||||||||||||||