Jesse Sartain Historical View

April 21st, 2010
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Historical View of Climate Change

Jesse Sartain Historical View By David Greenfield.

Many people don’t seem to realize that climate changes have been with us for a very long time. A common watershed mark is the beginning of the industrial era. If we look at pre-1780 we can see the following “drivers” or “forces” contributing to climate change: changes in the Earth’s orbit, changes in the Sun’s intensity, volcanic eruptions, changes in greenhouse gas concentrations and changes in ocean currents.

The Earth’s orbit does change, in terms of tilt and what are called “eccentricity” and “precession”. These affect the amount of sunlight striking the Earth’s surface. There are known fluctuations in the Sun’s intensity. These can cause both warming and cooling effects.

Solar activity affects both global warming and cooling. For example, reduced solar activity from the 1400s to the 1700s was a key factor in what came to be known as the “Little Ice Age”. This resulted in a cooling of North America, Europe and probably other parts of the globe.

Volcanoes are another “natural” cause of climate changes. It
is interesting to note that volcanoes emit aerosols and carbon dioxide. We don’t generally think of aerosols existing before aerosol cans.

The heating or cooling of the Earth can cause fluctuations in the heating or cooling of the Earth’s surface; this is the impetus for the current concern over emissions which are thought to contribute to the greenhouse gas effect. When global temperatures warm, carbon dioxide is released from the Earth’s oceans. This combined with changes to the Earth’s orbit trigger a warm or interglacial period, thereby increasing concentrations or levels of carbon dioxide. These increased levels amplify the warming effect by exacerbating the greenhouse effect.

If we look at the last 2,000 years we can conclude that the climate has been relatively stable. There have been three notable exceptions to this stability which scientists have labeled “the Medieval Climate Anomaly,” “the Little Ice Age” and “the Industrial Era.”

The so-called Medieval Anomaly is described as follows: between 900 and 1300 A.D. evidence suggests that Europe, Greenland and Asia experienced relative warmth. The exact magnitude, geographical regions and timing of these warming periods are uncertain. It is documented that the American West experienced very dry conditions during this time.

The Little Ice Age, as it was called, was sort of a misnomer, because it was not a true “Ice Age.” Major ice sheets did not develop, however, between 1500 and 1850, the average temperature of the Earth was possibly up to 2 degrees (Fahrenheit) colder than today, varying by region.

The Industrial Era is the anomaly we look at most closely today because another warming period has ensued over the last 100 years, coinciding with a substantial increase in emissions from human activity. According to the Environmental Protection Agency, starting around 1750, human activity began to add substantially to heat trapping greenhouse gases in the Earth’s atmosphere. Both the burning of fossil fuels and an increase in the Earth’s biomass, for example, has resulted in emissions of aerosols. These aerosols absorb and emit heat and simultaneously reflect light. The addition of greenhouse gases and aerosols in to the Earth’s atmosphere has created observed climate changes. Here are some of our current understandings as to why these changes have occurred:

First of all, land cover and land use change are cited. Changes in land surface can be just as important as changes to the atmosphere because of how much they affect the reflectivity of solar rays. Processes such as deforestation, reforestation, desertification and urbanization often contribute to changes in climate temperature, wind and precipitation. Changes in land cover and land use can also affect the amount of carbon dioxide taken up or released by the land surface. A whole science surrounding “carbon sequestration” has developed around these phenomena.

What is in store for the future? Greenhouse gas concentrations are expected to increase during the next century unless greenhouse gas emissions decrease significantly from present levels. These gas concentrations are expected to raise the Earth’s temperature, influence precipitation and create storm patterns which may raise sea levels. It is speculated that future climate changes will depend on the following: Whether there will be a continued increase in the production of greenhouse gases and aerosols. How strongly features of our climate respond to these concentrations. And lastly, how much the climate will vary due to natural influences such as the Sun’s intensity or volcanic activity. Another consideration is what is called the Earth’s “internal variability,” referring to random changes in the circulation of the Earth’s atmosphere and oceans.

We are currently producing virtual models of possible changes to the Earth’s atmosphere on computers. Climatologist calls these GCMs or General Circulation Models. According to the IPCC (Intergovernmental Panel on Climate Change) these models are thought to be “extremely important tools for simulating and understanding climate, and there is considerable confidence that they are able to provide credible quantitative estimates of future climate change, particularly at larger scales.

The entire subject of global warming is polarized between nations, political parties and economic interests. Even in the scientific community there is disagreement about man’s impact on the environment and what constitutes good science.

Experts are even disagreeing on points as basic as establishing a means for measuring either the global mean temperature or what is referred to as AGW, Anthropogenic Global Warming.

As early as 1989, the United Nations claimed that we were on a ten year countdown towards a “tipping point” wherein the global mean temperature was likely to rise above a 2 degree increase above pre-industrial levels, in which case, there was nothing we could do to reverse the eventual cataclysmic effects of global warming. Of course that was 21 years ago.

Russian critics of the Kyoto Protocol, which calls for cuts in CO2 emissions, say that the theory underlying the pact lacks scientific basis. The American Physical Society reports: There is a considerable presence within the scientific community of people who do not agree with the IPCC conclusion that anthropogenic CO2 emissions are very probably likely to be primarily responsible for the global warming that has occurred since the Industrial Revolution. Other detractors state that the global mean surface temperature has not risen since 1998 and may have fallen since late 2001.

Jesse Sartain Historical

Jesse Sartain Food Waste

April 21st, 2010
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How is Food Waste Adding to Global Warming and Poverty?

Jesse Sartain Food Waste by Stephen William.

There’s a simple way to reduce global warming and save money at the same time – don’t waste food.

In his book, ‘Waste – The Global Scandal’, Tristram Stuart, calculates that British households consign 5.4 million tonnes of edible food to the bin each year. That’s 25% of all the food that Britons eat at home. It hits them in the pocket as well. That means that it costs each British household, on average, £8 ($14) a week.

Stuart quotes some more amazing British food waste statistics. Among other other perfectly-edible items that go in the bin annually are:

- 2.6 billion (yes, billion!) slices of bread;

- £370 million worth of bananas;

- 1.6 billion uneaten apples;

- 484 million opened pots of yoghurt.

Unfortunately, the message of food waste has been passed to our children – about a third of school packed lunches end up in the bin.

The repercussions of this waste are serious on a global scale. The developed countries’ demand for food pushes up global food prices. In 2007, average global food prices rose by 23 per cent. By the following year, prices had gone up by a staggering 54 per cent.

This matters. The result of increased food prices is that up to an estimated 100 million extra people were pushed into chronic hunger. Chronic hunger in turn increases the child mortality rate amongst this group. It’s estimated, according to Stuart, that the rate has risen to 25 per cent.

And waste food contributes to the pressure on scarce land resources. 8.3 million hectares of land are needed to produce just the products wasted in the UK and the US. That’s seven times the amount of Brazilian rainforest that was destroyed in 2008 to produce food.

As food prices rise, the greater the financial incentive to deforest the rainforests. But they’re vital to deal with global warming.

So what can you do to reduce your food waste?

Don’t buy too many meat and dairy products at once. These products are more perishable than other foods and take up to four times more land to produce and result in more greenhouse gas emissions (particularly from cattle).

Use a shopping list. With the massive variety of foods available in the supermarkets, it’s easy to make impulse purchases. Make a list and stick to it. Only buy ‘buy one, get one free’ deals if it’s something that you regularly use and will finish.

Keep an eye on what’s in the fridge. Much food is wasted because we’ve forgotten that it’s in the fridge or cupboard.

Jesse Sartain Food

Do Something with Jesse Sartain

April 21st, 2010
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Global Warming is Real and We Can Do Something About It

Do Something with Jesse Sartain By Cheryl Forbes.

It is time that we care about Mother Earth. Anything that happens to her, happens to all of us. Nobody is spared. This might be grim but it is the truth. One of the greatest worries of Mother Earth is global warming. Kids are taught about Global Warming in school. It can also be seen at children television shows. Integrated with the show’s theme. Even parks and museums show the devastating effects of global warming, informing not only the kids but the adults too.

Global warming is a large responsibility for one man to carry alone. But if all of us would care enough to change our lifestyles, then it would make a difference. Change it in such a way that our lifestyle will no longer contribute to the rising temperature of the Earth’s atmosphere. We can make it happen. We can make a difference especially if we do it together.

A few of the effects of global warming are the increase in sea levels because of the melting ice over at the Antarctica region, erratic changes in the weather, floods, typhoons, hurricanes, forest fires, etc.

We need to be shaken awake from the deep slumber that we are in because even if we have been informed of the effects and causes of global warming. It would seem that we do not care enough to change our ways. Simple change in our lifestyle is all that would take to gradually decrease global warming. The past is behind us and we can no longer do something about it. The future we can still change. So let us do our part and be responsible not only to ourselves but to others too.

Something with Jesse Sartain