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Green FAQ's
Green FAQ's


What is the role of renewable energy to climate change?

How is Carbon dioxide a greenhouse gas?

Is the climate becoming more variable or extreme?


Question What is the role of renewable energy to climate change?

  • Energy use from fossil fuel is the dominant source of greenhouse gas emissions made by man. If we could produce all our energy from renewable sources tomorrow we would have very little problem with climate change, according to some sources. Nature produces 94 to 96% of all CO2 and over 99% of all greenhouse gases. Without these gases the planet would die and be extremely cold. Man is currently blamed, by some, for causing 0.01% of the atmospheric change. (280ppm to 380ppm). This number is irrationally high, we will discuss the issue shortly.

    With the exception of hydroelectric, no "renewable energies are currently able to provide any actual power. Most are similar to wind in that the variations are so great and the actual output so small that they produce no effective power. Most systems provide so little that they can't even reproduce themselves with the total expected output of a given system. It takes more then 100% of all power that is ever expected to come out of a wind system to build another, plus so extra power. They, like solar panels, should be banned as an energy waste. We could make a step towards fossil fuel reduction just by stopping the creation of these energy wasting devices.



Question How is Carbon dioxide a greenhouse gas?

  • CO2 is a greenhouse gas because it increases the temperature level of the earth in the same way the heat is generated inside the greenhouse where plants are grown. Greenhouses or glass houses trap the heat within thereby increasing the temperature within the glasshouse. In the same way, CO2 acts like a blanket in the earth atmosphere and prevents the heat from escaping from the earth's surface, leading to a rise in global temperatures.



Question Is the climate becoming more variable or extreme?

  • Examination of changes in climate extremes requires long-term daily or even hourly data sets which until recently have been scarce for many parts of the globe. However these data sets have become more widely available allowing research into changes in temperature and precipitation extremes on global and regional scales. Global changes in temperature extremes include decreases in the number of unusually cold days and nights and increases in the number of unusually warm days and nights. Other observed changes include lengthening of the growing season, and decreases in the number of frost days.

    Global temperature extremes have been found to exhibit no significant trend in interannual variability, but several studies suggest a significant decrease in intra-annual variability. There has been a clear trend to fewer extremely low minimum temperatures in several widely-separated areas in recent decades. Widespread significant changes in extreme high temperature events have not been observed. There is some indication of a decrease in day-to-day temperature variability in recent decades.

    In areas where a drought or excessive wetness usually accompanies an El Niño or La Niña, these dry or wet spells have been more intense in recent years. Further, there is some evidence for increasing drought worldwide, however in the U.S. there is no evidence for increasing drought.In some areas where overall precipitation has increased (ie. the mid-high northern latitudes), there is evidence of increases in the heavy and extreme precipitation events. Even in areas such as eastern Asia, it has been found that extreme precipitation events have increased despite total precipitation remaining constant or even decreasing somewhat. This is related to a decrease in the frequency of precipitation in this region.

    Many individual studies of various regions show that extra-tropical cyclone activity seems to have generally increased over the last half of the 20th century in the northern hemisphere, but decreased in the southern hemisphere. Furthermore, hurricane activity in the Atlantic has shown an increase in number since 1970 with a peak in 2005. It is not clear whether these trends are multi-decadal fluctuations or part of a longer-term trend.




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