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Climate Change - An Object Presentation of Facts and Issues

Natural Causes of Climate Change

When most people hear the phrase climate change, they immediately think "atmospheric carbon".  But this is a gross over-simplification of the factors that result in the temperature on earth's surface  There are many other factors also at work, and in complex ways.  Current models to predict climate changes have been demonstrated to be consistent only in their unreliability. In the 70's a global ice age was predicted, then "global warming" and now, to avoid facing the unpredictability of their models, many of these same scientists now simply call it "climate change".

But the climate has always been change, long before humanity even existed. Here's why: the earth’s climate is affected by and changed through many natural causes like volcanic eruptions, ocean currents, movement of tectonic plates, the Earth’s orbital changes, solar variations and internal variability.volcanic emissions and climate change

Volcanic eruptions

The primary effect volcanoes have on the climate is short-term cooling. Volcanic eruptions pump out clouds of dust, gases and ash, which block out some sunlight.

Volcanic ash

Because the ash particles are relatively heavy, they fall to the ground within about three months, so their cooling effect is very short-lived.

Volcanic gases

Volcanic emissions also includes gases, like sulfur dioxide. SO2 combines with water vapor and dust in the atmosphere to form sulfate aerosols, which reflect sunlight away from the Earth’s surface. These aerosols are lighter than ash particles and can remain in the atmosphere for a year or more. Their cooling effect outweighs the warming caused by volcanic greenhouse gases; the eruption of Mount Pinatubo in 1991 caused a 0.5 °C drop in global temperature. The atmospheric SO2 can also produce acid rain, which can result in deforestation, which also then affects weather patterns and atmospheric CO2.

In addition to ash and lave, volcanic eruptions spew out carbon dioxide (CO2).  As carbon in natural sources (such as coal and oil deposits) is moved by tetonic plate movement into a volcano or ocean rift, it is again brought to the surface and atmosphere.

And CO2 does have a warming effect. The average volcanic CO2 emissions are generally small compared to CO2 produced by human activity, but there can be exceptions, like a major eruption. In normal times, volcanic CO2 is thought to be less than 1% of emissions from current human activities. .

Large volumes of gases and ash can influence climatic patterns for years by increasing planetary reflectivity causing atmospheric cooling.

Asteroid and meteorite strikes

Of course, most people recall learning that an asteroid strike is believed by scientists to have caused such profound climate change that it brought about the end of the dinosaurs. An impact from an object 10km across could:
release huge quantities of vaporized material into the atmosphere, blocking out the Sun;

  • Cause a shock wave for hundreds of miles
  • Earths Orbital cyclesProduce firestorms for thousands of miles
  • Rain debris containing the iridium coating plants
  • Create globally distributed acid rains.

See this page for more information.

Earth orbital cycles

 Shifts and wobbles in the Earth’s orbit can trigger changes in climate such as the beginning and end of ice ages. The last ice age ended about 12,000 years ago and the next cooling cycle may begin in about 30,000 years. But orbital changes are so gradual they’re only noticeable over thousands of years; not decades or centuries.

The earth makes one full orbit around the sun each year. It is tilted at an angle of 23.5° to the perpendicular plane of its orbital path. Changes in the tilt of the earth can lead to small but climatically important changes in the strength of the seasons, more tilt means warmer summers and colder winters; less tilt means cooler summers and milder winters.

Slow changes in the Earth’s orbit lead to small but climatically important changes in the strength of the seMilankovitch cyclesasons over tens of thousands of years. Climate feedbacks amplify these small changes, thereby producing ice ages.

The Milankovitch cycles include:

  1. The shape of Earth’s orbit, known as eccentricity;
  2. The angle Earth’s axis is tilted with respect to Earth’s orbital plane, known as obliquity; and
  3. The direction Earth’s axis of rotation is pointed, known as precession

And here's a deeper explanation of each of these:

  • Precession: a 26,000-year shift in the orientation of Earth’s axis of rotation that affects how much summer sun is received at high latitudes (and shifting how much reaches the north vs south).
  • Obliquity: a 41,000-year change in the tilt of the Earth’s axis relative to the sun that changes how much sun is received during a year at the poles versus the equator.
  • Eccentricity: a 100,000-400,000 change in the shape of the Earth’s orbit around the sun that alters the length of the seasons and affects the importance of precession.


Ocean currentsOcean currents and earth's temperature

The oceans are a major component of the climate system. Ocean currents are located at the ocean surface and in deep water below 300 meters (984 feet). They can move water horizontally and vertically and occur on both local and global scales. The ocean has an interconnected current, or circulation, system powered by wind, tides, the Earth’s rotation (Coriolis effect), the sun (solar energy), and water density differences. The topography and shape of ocean basins and nearby landmasses also influence ocean currents. These currents depend on many factors, including the salinity of the sea water and tectonic plate movements (at some point in the future, Europe and North America will move too far apart for the current to be sustained).

Deep ocean currents are density-driven and differ from surface currents in scale, speed, and energy.

Water density is affected by the temperature, salinity (saltiness), and depth of the water.

The colder and saltier the ocean water, the denser it is. The greater the density differences between different layers in the water column, the greater the mixing and circulation. Density differences in ocean water contribute to a global-scale circulation system, also called the global conveyor belt The global conveyor belt includes both surface and deep ocean currents that circulate the globe in a 1,000-year cycle.

This circulation is the result of two simultaneous processes:

  • warm surface currents carrying less dense water away from the Equator toward the poles, and
  • cold deep ocean currents carrying denser water away from the poles toward the Equator.

The ocean’s global circulation system plays a key role in distributing heat energy, regulating weather and climate, and cycling vital nutrients and gases.

Solar variations

 The Sun is the source of energy for the Earth’s climate system. Although the Sun’s energy output appears constant from an everyday point of view, small changes over an extended period of time can lead to climate changes.

Some scientists suspect that a portion of the warmsolar-caused temperature variationsing in the first half of the 20th century was due to an increase in the output of solar energy. As the sun is the fundamental source of energy that is instrumental in our climate system it would be reasonable to assume that changes in the sun's energy output would cause the climate to change.

Scientific studies demonstrate that solar variations have performed a role in past climate changes. For instance a decrease in solar activity was thought to have triggered the Little Ice Age between approximately 1650 and 1850, when Greenland was largely cut off by ice from 1410 to the 1720s and glaciers advanced in the Alps. Current global warming however cannot be explained by solar variations.

Since 1750, the average amount of energy coming from the Sun either remained constant or increased slightly. If global warming was caused by a more active sun, scientists presently believe this would cause warmer temperatures in all layers of the atmosphere. They have only observed a cooling in the upper atmosphere, a warming at the surface and in the lower parts of the atmosphere.

This is believed to be due to greenhouse gases capturing heat in the lower atmosphere. Also climate models that include solar irradiance changes cannot reproduce last century's observed temperature trend without including a rise in greenhouse gases.

Large scale forest fires and deforestation

Large scale fires release considerable amounts of carb and particulates while simultaneously removing living plants that remove carbon and produce oxygen; a double whammy for the earth's carbon cycle.

Natural erratic variation

 Some changes in climate have no external trigger. These changes are instead caused by interactions within the climate system itself, often involvEl Nino, El Ninaing positive feedbacks.

One example is the El Niño–La Niña cycle, which can cause temporary warming and cooling. Both phenomena affect atmospheric circulation patterns and influence global climate. While El Niño increases global temperature, La Niña decreases it. This cycle repeats itself on a timescale of about five years. But these changes are short-term, only lasting a few years.

Another example of internal variability is the Arctic oscillation (AO), which is associated with changing patterns of air pressure in the northern hemisphere.

This phenomenon brings warmer weather to parts of Europe and North America, leaving the Arctic colder than usual. The other phase of the AO brings the opposite conditions, resulting in a warmer-than-usual Arctic and colder weather in the sub-polar regions. Because of this seesaw effect, the AO has little effect on global temperatures, but can significantly Artic oscillationinfluence local and regional weather.

Many natural factors affect the climate, including changes in the Sun’s output or the Earth’s orbit, large volcanic eruptions and internal variability such as El Niño. Scientists measure these effects, but none can account for the observed trend since 1970.

Methane and CO2 produced by other natural sources

Methane is produce by animals (burping bovine), decay of plant matter in forests, swamps and other natural sources. CO2 gets all the attention lately, but methane also impacts how the earth absorbs and reflects solar radiation. Methane is considered to be 100 times worse than carbon dioxide due to it's effect on greenhouse warming. 

 According to NASA, about 30% of methane emissions are produced by wetlands, including ponds, lakes, and rivers. Another 20% is produced by agriculture, due to a combination of livestock, waste management and rice cultivation. Activities related to oil, gas, and coal extraction release an additional 30%. The remainder of methane emissions come from minor sources such as wildfire, biomass burning, permafrost, termites, dams, and the ocean.

Ocean absorption and release of heat and gases The natural carbon cycle

Every 5th grader knows the oceans cover 75% of the earth's surface.  Water absorbs and releases heat more slowly that land. So, oceans can act as a heat sink, absorbing and releasing heat from solar radiation. 

Plant and animal life in the oceans affects the carbon cycle, which then impacts temperatures. 

  • Ocean algae produce oxygen : Scientists estimate that 50 to 80% of the oxygen production on Earth comes from the ocean. The majority of this production is from oceanic plankton such as drifting plants, algae, and some bacteria that can photosynthesize.
  • Stromatalytes can absorb CO2 producing calcium carbonate, removing it from the atmosphere.

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