Floodstones to help predict climate change

A slight problem in England could be that parts of the south e.g. London have been slowly sinking into the clay for centuries, so readings might not tell the whole story. When it comes to predicting climate change, most scientists use state-of-the-art supercomputers to model future trends. But researchers at the University of Sheffield are […]

via Ancient floodstones sought to help predict climate change — Tallbloke’s Talkshop

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Nabarup Ganguly- Effects of Climate On Agriculture

Agriculture is the basic activity by which humans live and survive on the earth. Assessing the impacts of climate change on agriculture is a vital task. In both developed and developing countries, the influence of climate on crops and livestock persists despite irrigation, improved plant and animal hybrids and the growing use of chemical fertilizers. The continued dependence of agricultural production on light, heat, water and other climatic factors, the dependence of much of the world’s population on agricultural activities, and the significant magnitude and rapid rates of possible climate changes all combine to create the need for a comprehensive consideration of the potential impacts of climate on global agriculture.

THE INFLUENCE OF CLIMATE CHANGE ON CROP PRODUCTION

At the basis of any understanding of climate impacts on agriculture lies the biophysical sciences. The rates of most biophysical processes are highly dependent on climate variables such as radiation, temperature, and moisture, that vary regionally. For example, rates of plant photosynthesis depend on the amount of photosynthetically active radiation and levels of atmospheric carbon dioxide (C02). Temperature is an important determinant of the rate at which a plant progresses through various phenological stages towards maturity. The accumulation of biomass is constrained by the availability of moisture and nutrients to a growing plant.

Numerous studies have examined the impacts of past climatic variations on agriculture using case studies, statistical analyses and simulation models (e.g. Nix 1985; Parry 1978; Thompson 1975; World Meteorological Organization 1979). Such studies have clearly demonstrated the sensitivity of both temperate and tropical agricultural systems and nations to climatic variations and changes. In the temperate regions, the impacts of climate variability, particularly drought, on yields of grains in North America and the Soviet Union have been of particular concern because of their effects on world food security. In the tropics, drought impacts on agriculture and resulting food shortages have been widely studied, especially when associated with the failure of the monsoon in Asia or the rains in Sudano-Sahelian Africa. In the temperate regions, climatic variations are associated with economic disruptions; in the tropics, droughts bring famine and widespread social unrest (Pierce 1990).

GLOBAL ESTIMATES OF AGRICULTURAL IMPACTS

Global estimates of agricultural impacts have been fairly rough to date, because of lack of consistent methodology and uncertainty about the physiological effects of CO2. General studies of how climate change might affect agriculture include those of the National Defense University (1983), Liverman (1986), and Warrick (1988). Kane et al. (1989) broadly predicted improvements in agricultural production at high latitudes and reductions in northern hemisphere mid-continental agricultural regions. The IPCC (199Ob) concluded that while future food production should be maintained, negative impacts were likely in some regions, particularly where present-day vulnerability is high.

An international project of the US Environmental Protection Agency (EPA), “Implications of Climate Change for International Agriculture: Global Food Trade and Vulnerable Regions,” has been established to estimate the potential effects of greenhouse gas-induced climate change on global food trade, focusing on the distribution and quantity of production of the major food crops for a consistent set of climate change scenarios and CO2 physiological effects. Other goals of the project are to determine how currently vulnerable, food-deficit regions may be affected by global climate change; to identify the future locations of those regions and the magnitudes of their food-deficits; and to study the effectiveness of adaptive responses, including the use of genetic resources, to global climate change.

As part of the EPA project, crop specialists are estimating yield changes at over 100 sites in over 20 countries  under common climate change scenarios using compatible crop growth models. The focus is on staple food crops: wheat, rice, maize, and soybeans. The crop models are those developed by the International Benchmark Sites Network for Agrotechnology Transfer (IBSNAT, 1990)—a global network of crop modelers funded by the U.S. Agency for International Development. The choice of the IBSNAT crop models was based on several criteria. First, the models simulate crop response to the major climate variables of temperature, precipitation, and solar radiation, and include the effects of soil characteristics on water availability for crop growth. Second, the models have been validated for a range of soil and climate conditions. Third, the models are developed with compatible data structures so that the same soil and climate data bases could be used with all crops.

Preliminary national production changes for wheat based on IBSNAT crop model (Rosenzweig and Iglesias, et al., 1992). Results from individual sites have been aggregated according to rainfed and irrigated practice and contribution to regional and national production. The table shows national production changes for the three climate change scenarios with (555 ppm) and without (330 ppm) the physiological effects of CO2 on crop growth.

In general, these results show that the climate change scenarios without the physiological effects of CO2 cause decreases in estimated national production, while the physiological effects of CO2 mitigate the negative effects. Production declines occur in many locations, however, even with the compensating CO2 effects. Production changes tend to be less negative and even positive in some cases in countries in mid and high latitudes, while simulations in countries in the low latitudes indicate more detrimental effects of climate change on agricultural production. The UKMO climate change scenario (mean global warming of 5.2deg.C) generally causes the largest production declines, while the GFDL and GISS (4.0 and 4.2deg.C mean global warming, respectively) production changes are more moderate.

When embedded in a global agricultural food trade model, the Basic Linked System (Fischer et al., 1988), the production change estimates based on IBSNAT crop model results will allow for projection of potential impacts on food prices, shifts in comparative advantage, and altered patterns of global trade flows for a suite of global climate change, population, growth, and policy scenarios.

CONCLUSIONS

In general, the tropical regions appear to be more vulnerable to climate change than the temperate regions for several reasons. On the biophysical side, temperate C3 crops are likely to be more responsive to increasing levels of CO2. Second, tropical crops are closer to their high temperature optima and experience high temperature stress, despite lower projected amounts of warming. Third, insects and diseases, already much more prevalent in warmer and more humid regions, may become even more widespread.

Tropical regions may also be more vulnerable to climate change because of economic and social constraints. Greater economic and individual dependence on agriculture, widespread poverty, inadequate technologies, and lack of political power are likely to exacerbate the impacts of climate change in tropical regions.

In the light of possible global warming, plant breeders should probably place even more emphasis on development of heat- and drought-resistance crops. Research is needed to define the current limits to these resistances and the feasibility of manipulation through modern genetic techniques. Both crop architecture and physiology may be genetically altered to adapt to warmer environmental conditions. In some regions it may be appropriate to take a second look at traditional technologies and crops as ways of coping with climate change.

At the regional level, those charged with planning for resource allocation, including land, water, and agriculture development should take climate change into account. In coastal areas, agricultural land may be flooded or salinized; in continental interiors and other locations, droughts may increase. These eventualities can be dealt with more easily if anticipated.

As climatic factors change, a host of consequences will ripple through the agricultural system, as human decisions involving farm management, grain storage facilities, transportation infrastructure, regional markets, and trade patterns respond. For example, field-level changes in thermal regimes, water conditions, pest infestations, and most importantly, quantity and quality of yields, may lead to changes in farm management decisions based on altered risk assessments. Consequences of these management decisions could result in local and regional alterations in farming systems, land use, and food availability. Ultimately, impacts of climate change on agriculture may reverberate throughout the international food economy and global society.

At the national and international levels, the needs of regions and people vulnerable to the effects of climate change on their food supply should be addressed. In many cases, reducing vulnerability to current climate variability should also serve to mitigate the impacts of global warming.

Fracking Britain – The Facts

The UK Prime Minister, David Cameron, is convinced that ‘fracking’ – or hydraulic fracturing – of shale gas and oil is the answer to the country’s energy supply worries and economic troubles. However politicians such as Caroline Lucas, environmental groups and thousands of local protesters are more than aware of the downsides to this ‘dash for gas’ and are desperate to shout about them loud and clear. So what is fracking, what are the benefits and what are the risks?

Horizontal hydraulic fracturing is an intensive method of fossil fuel extraction. Where gas or oil lies within the earth in layers or shales, there is the possibility of extracting it by pumping sand, chemicals and a huge amount of water into the shale and letting the fuel come up into a well. The horizontal method is new while conventional oil or gas drilling is vertical. The US has recently undergone a huge ‘fracking revolution’ and the UK has granted over 100 licenses for exploratory drilling while other countries such as China and Poland are also in the process of undergoing this process.

The benefits of fracking are largely the benefits to any kind of fossil fuel extraction. Our whole economy is powered by fossil fuel, so nations are always desperate to pull more and more out of the ground – especially as oil extraction around the world starts to decline. For the UK specifically, fracking would create a lot of profit, helping our economy to grow. It will also create jobs, and possibly improve our energy security, although this isn’t definite because the companies that frack will actually just sell the fuel to the highest bidder in Europe – as the whole EU has an integrated energy supply system.  Cameron claims it will lower domestic gas bills – but there is evidence to the contrary. Caudrilla itself – one of the biggest companies involved – has admitted that the effect on gas bills will be marginal, if anything.

So there are some economic benefits. But there are many downsides. First off, this ‘dash for gas’ completely contradicts the 2008 Climate Change Act, as the continual investment in fossil fuels not only pollutes the atmosphere and deepens the climate change problem, it also diverts investment potential and public spending away from renewable energy technology.
There is also a risk of earth tremors – tiny earthquakes – caused by fracking sites. This happened at an exploratory site near Blackpool, causing significant public concern.
Fracking also has significant health risks, as the gas and chemicals can (and often do) leak into the groundwater of the area. This will not only put aquatic wildlife in jeopardy, but can also contaminate local drinking water. If this happens, the health and safety risks to local people are severe.
The industrialisation of the countryside is also an issue to many people who live in rural communities. Huge noisy trucks chugging through small villages create traffic congestion and localised atmospheric pollution.
The aesthetic value of the English landscape is also damaged by industrial fracking plants. Not only is this a shame in itself, but it will also lower local house prices, which in turn will have a negative economic effect on local areas. Households very near to a site may even have trouble getting house insurance.

At the moment both government and the public are massively divided on the fracking debate. It’s proving to be a very controversial issue, with campaign groups such as Frack Free Somerset and Frack Free Sussex cropping up to organise the opposition.  The testing site in Balcomb, Sussex, has seen thousands of protesters from both the local area and all over the country camping out for days on end, desperate for their views to be taken seriously.

Anti-fracking protest at Balcomb. Image from the Guardian.

Anti-fracking protest at Balcomb. Image from the Guardian.

If he’s serious about democracy, David Cameron will listen to the people rather than the pound signs. Is that really too much to ask for?

Resources:

http://ecowatch.com/2013/fracking-protests-intensify-officials-push-drilling/

http://www.greenpeace.org.uk/newsdesk/energy/fact-check/will-fracking-lower-bills

http://www.independent.co.uk/news/uk/politics/fracking-the-great-debate-8782853.html

Climate Change: Issues of Magnitude and Pace

The planet is undergoing one of the largest changes in climate since the dinosaurs went extinct. But what might be even more troubling for humans, plants and animals is the speed of the change. Stanford climate scientists warn that the likely rate of change over the next century will be at least 10 times quicker than any climate shift in the past 65 million years.

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