River Dart fisheries survey 1974

This is the River Dart Fisheries Survey 1974 report produced by the South West Water Authority. The survey was carried out between July and October 1974 to assess the extent of the 0+ and 1+ Salmo salar L. population in the Dart catchment and thereby assess directly the success of the 1973/74 and 1972/73 spawning season. The survey showed that there were large numbers of salmon parr distributed throughout the upper reaches of the Dart, reflecting the successful spawning of the 1973/74 and 1972/73 season. It contains tables with survey sections locations, presence/absence for each section and location maps with spawning grounds and sampling stations

Forty years of linking orbits to ice ages

In 1976, it was demonstrated that tiny wobbles in Earth’s orbit led to the great ice age cycles of the past few million years. This finding had wide implications for climate science and the details remain hotly debated today

Chronology for climate change: Developing age models for the biogeochemical ocean flux study cores

We construct age models for a suite of cores from the northeast Atlantic Ocean by means of accelerator mass spectrometer dating of a key core, BOFS 5K, and correlation with the rest of the suite. The effects of bioturbation and foraminiferal species abundance gradients upon the age record are modeled using a simple equation. The degree of bioturbation is estimated by comparing modeled profiles with dispersal of the Vedde Ash layer in core 5K, and we find a mixing depth of roughly 8 cm for sand-sized material. Using this value, we estimate that age offsets between unbioturbated sediment and some foraminifera species after mixing may be up to 2500 years, with lesser effect on fine carbonate (<10 mu m) ages. The bioturbation model illustrates problems associated with the dating of ''instantaneous'' events such as ash layers and the ''Heinrich'' peaks of ice-rafted detritus. Correlations between core 5K and the other cores from the BOFS suite are made on the basis of similarities in the downcore profiles of oxygen and carbon isotopes, magnetic susceptibility, water and carbonate content, and via marker horizons in X radiographs and ash beds

Northeastern Atlantic benthic foraminifera during the last 45,000 years: Changes in productivity seen from the bottom up

We studied benthic foraminifera from the last 45 kyr in the >63 mu m size fraction in Biogeochemical Ocean Flux Studies (BOFS) cores 5K (50 degrees 41.3'N, 21 degrees 51.9'W, depth 3547 m) and 14K (58 degrees 37.2'N, 19 degrees 26.2'W, depth 1756 m), at a time resolution of several hundreds to a thousand years. The deepest site showed the largest fluctuations in faunal composition, species richness, and benthic foraminiferal accumulation rates; the fluctuations resulted from changes in abundance of Epistominella exigua and Alabaminella weddellensis. In the present oceans, these species bloom opportunistically when a spring plankton bloom results in seasonal deposition of phytodetritus on the seafloor. The ''phytodetritus species'' had very low relative abundances and accumulation rates during the last glacial maximum. A strong increase in absolute and relative abundance of E. exigua and A weddellensis during deglaciation paralleled the decrease in abundance of the polar planktonic foraminifer Neogloboquadrina pachyderma (s), and the increase in abundance of warmer water planktonic species such as Globigerina bulloides. This strong increase in relative abundance of the ''phytodetritus species'' and the coeval increase in benthic foraminiferal accumulation rate were thus probably caused by an increase in the deposition of phytodetritus to the seafloor (and thus probably of surface productivity) when the polar front retreated to higher latitudes. The abundance of ''phytodetritus species'' decreased during the Younger Dryas, but not to the low levels of fully glacial conditions. During Heinrich events (periods of excessive melt-water formation and ice rafting) benthic accumulation rates were very low, as were the absolute and relative abundances of the ''phytodetritus species'', supporting suggestions that surface productivity was very low during these events. In both cores Pullenia and Cassidulina species were common during isotope stages 2, 3 and 4, as were bolivinid, buliminid and uvigerinid species. High relative abundances of these species have been interpreted as indicative either of sluggish deep water circulation or of high organic carbon fluxes to the seafloor. In our cores, relative abundances of these species are negatively correlated with benthic foraminiferal accumulation rates, and we can thus not interpret them as indicative of increased productivity during glacials. The percentage of these ''low oxygen'' species calculated on a ''phytodetritus species'' - free basis decreased slightly at deglaciation at 5K, but not at 14K. This suggests that decreased production of North Atlantic Deep Water during the last glacial might have slightly affected benthic foraminiferal faunas in the eastern North Atlantic at 3547 m depth, but not at 1756 m. In conclusion, major changes in deep-sea benthic foraminiferal faunas over the last 45,000 years in our cores from the northeastern Atlantic were the result of changes in surface water productivity, not of changes in deep water circulation; productivity was lower during the glacial, probably because of extensive ice cover

Putting the United Nations Sustainable Development Goals into practice: A review of implementation, monitoring, and finance

In January 2016, after two years of international negotiations, the Sustainable Development Goals (SDGs) came into effect. The SDGs are the successors to the Millennium Development Goals (MDGs) and represent an ambitious but potentially flawed agenda for sustainable development through to 2030. This review assesses the legacy of the MDGs, the development of the SDGs, and the international framework to put the SDGs into practice. We propose dividing the framework for SDG delivery into three key areas: implementing the goals and the SDG agenda (Implementation); monitoring, evaluation, and review (Monitoring); and increasing and improving global finance flows for sustainable development (Finance). This review identifies the challenges faced by the international community for making the SDGs an effective platform for equitable and sustainable development across these three areas. Proposed approaches and solutions are discussed and further research is suggested. This review concludes that further critical attention to the “Implementation”, “Monitoring”, and “Finance” framework is vital to ensure accountability and transparency from an ever‐growing number of state and non‐state development actors. This review also seeks to further the potential for greater links between development theory, development geography, and development actors and institutions to improve development under the SDGs and increase engagement from geography on the SDGs. This framework points towards a basis for critical engagement on the sustainability, equality, and quality of development, while challenging the primacy of economic growth‐based paradigms in SDG implementation

The politics of the anthropocene: a dialogue

This paper stages a dialogue between a human geographer and a physical geographer about the concept of the Anthropocene. The aim of the dialogue is not to arrive at an agreement about how the Anthropocene should be defined, but rather to open up the question of the politics of the concept and its definition. The dialogue revolves around three issues: (1) the politics of the debate about the geoscientific definition of the Anthropocene Epoch; (2) the relation between the geoscientific debate about the Anthropocene and the burgeoning literature on the Anthropocene in the social sciences and humanities, including human geography; (3) the relation between geoscientific and political concepts

Distribution of climate suitability for viticulture in the United Kingdom in 2100

Changes in temperature of the second half of the 20th Century led to significant changes in the areas of the UK suitable for high-quality viticulture. A warming climate and acceptable rainfall levels (although not without a number of risks to harvest yields) has made it possible for UK wine producers to produce high quality sparkling wine in the so-called ‘golden triangle’ south of London. As the climate continues to change over the course of the 21st century through to 2100, the possibilities for UK viticulture will again continue to shift. While rising temperatures bring warmer growing seasons that may create potential opportunities for grape varieties that are currently widely planted in Europe to be grown in the UK, as well as having the potential to reduce the risk of spring frosts that inhibit bud growth, warmer climate conditions in the UK also bring a number of threats to UK wine growers. Chief amongst these threats are the increases in rainfall and the increasing risk of extreme weather events. For the long-term development of UK viticulture, it is important to assess a range of possible climate futures for 2100. The potential for significant changes to climatic conditions will require long term changes in strategy, skills and human capital development and significant further research to mitigate risks and identify potential opportunities from adapting UK viticulture to climate change. We have analysed one potential climate change scenario based on three key variables for growing high quality wine grapes, based on a ‘middle-of-the-road’ projection of changing temperatures and rainfall for the UK for 2100 due to climate change. Overall our findings suggest that, according to our estimates, that the UK may become an ‘intermediate climate’ wine region by 2100. It is currently a marginal, coolclimate region. However, some of the areas of the south of England may become either too hot, too wet, or both, to grow quality wine grapes in 2100

Life cycle assessment synthesis of the carbon footprint of Arabica coffee: Case study of Brazil and Vietnam conventional and sustainable coffee production and export to the United Kingdom

Over 9.5 billion kg of coffee is produced annually and demand is expected to triple by 2050. Hence, the identification and quantification of the greenhouse gas emission footprint of coffee is essential if it is to become a more sustainable crop. We have produced a detailed life cycle assessment of the carbon equivalent footprint of coffee produced in Brazil and Vietnam and exported to the United Kingdom. The average carbon footprint of Arabica coffee from both countries was calculated as 15.33 (±0.72) kg of carbon dioxide equivalent per 1 kg of green coffee (kg CO2e kg−1 ) for conventional coffee production and 3.51 (±0.13) kg CO2e kg−1 for sustainable coffee production. The 77% reduction in carbon footprint for sustainable coffee production in comparison to conventional production was due to exportation of coffee beans via cargo ship rather than freight flight and the reduction of agrochemical inputs. Based on our results, further reductions could be made through optimal use of agrochemicals; reduced packaging; more efficient water heating; renewable energy use; roasting beans before exportation; and carbon offsetting. Applying these recommendations correctly through certification schemes could mitigate other environmental impacts of coffee cultivation

Estimating the scale of the US green economy within the global context

Article Open Access Published: 15 October 2019 Estimating the scale of the US green economy within the global context Lucien Georgeson & Mark Maslin Palgrave Communications volume 5, Article number: 121 (2019) | Download Citation Article metrics 2020 Accesses 194 Altmetric Metricsdetails Abstract The green economy has previously been defined and measured in various, but limited, ways. This article presents an estimation of the scale of and employment in the US Green Economy using a data triangulation approach that uses many sources of data and multiple types of data. This can give a suggestion of the green economy’s role in economic development and employment at the country level. It also makes it possible to compare the scale of ‘green jobs’ to employment in fossil fuel-related sectors, and to compare the US green economy to other economies. Through the Low Carbon and Environmental Goods and Services Sector (LCEGSS) dataset, the US green economy is estimated to represent $1.3 trillion in annual sales revenue and to employ nearly 9.5 million workers; both of which have grown by over 20% between 2012/13 and 2015/16. Comparison with China, OECD members and the G20 countries suggests that the US is estimated to have a greater proportion of the working age population employed (4%) and higher sales revenue per capita in the green economy. Estimated values for other countries suggests that they too have significant production and consumption in the green economy and the US should consider, as other economies are, developing energy, environmental and educational policies relevant to the green economy to remain competitive in these areas. Given the shortcomings of other data sources, this information can contribute to understanding the potential impact of changes to federal-level policies on economic sectors that are vital to combating climate change and protecting the environment

Global disparity in the supply of commercial weather and climate information services

Information about weather and climate is vital for many areas of decision-making, particularly under conditions of increasing vulnerability and uncertainty related to climate change. We have quantified the global commercial supply of weather and climate information services. Although government data are sometimes freely available, the interpretation and analysis of those data, alongside additional data collection, are required to formulate responses to specific challenges in areas such as health, agriculture, and the built environment. Using transactional data, we analyzed annual spending by private and public organizations on commercial weather and climate information in more than 180 countries by industrial sector, region, per capita, and percentage of GDP (gross domestic product) and against the country's climate and extreme weather risk. There are major imbalances regarding access to these essential services between different countries based on region and development status. There is also no relationship between the level of climate and weather risks that a country faces and the level of per capita spending on commercial weather and climate information in that country. At the international level, action is being taken to improve access to information services. With a better understanding of the flows of commercial weather and climate information, as explored in this study, it will be possible to tackle these regional and development-related disparities and thus to increase resilience to climate and weather risks