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We are not seeing large changes in ocean currents. We are not seeing an increase in solar radiation. We are, however, seeing an increase in anthropogenic CO2. It is known that increasing CO2 leads to increased radiative forcing. It is known that increased radiative forcing must result in higher temperatures. It is known that such increase can lead to feedback effects, enhancing the anthropogenic effect.
The cause of the glacial to interglacial increase in atmospheric carbon dioxide is now thought to be due to changes in ventilation of deep water at the ocean surface around Antarctica and the resulting effect on the global efficiency of the “biological pump”.6
The above mechanism for glacial to interglacial variation in carbon dioxide concentration is supported by the observation that the rise in carbon dioxide lags the temperature increase by some 800-1000 years—ruling out the possibility that rising carbon dioxide concentrations were responsible for terminating glacial periods. As a consequence, it is now generally believed that glacial periods are terminated by increased insolation in polar regions due to quasi-periodic variations in the Earth’s orbital parameters. And it is true that paleoclimatic archives show spectral components that match the frequencies of Earth’s orbital modulation.
Thanks to new calculations by a Dartmouth geochemist, scientists are now looking at the earth's climate history in a new light.
Mukul Sharma, Assistant Professor of Earth Sciences at Dartmouth, examined existing sets of geophysical data and noticed something remarkable: the sun's magnetic activity is varying in 100,000-year cycles, a much longer time span than previously thought, and this solar activity, in turn, may likely cause the 100,000-year climate cycles on earth. This research helps scientists understand past climate trends and prepare for future ones.
Published in the June 10 issue of Earth and Planetary Science Letters (Elsevier, volume 199, issues 3-4), Sharma's study combined data on the varying production rates of beryllium 10, an isotope found on earth produced when high-energy galactic cosmic rays bombard our atmosphere, and data on the past variations in the earth's magnetic field intensity. With this information, Sharma calculated variations in solar magnetic activity going back 200,000 years, and he noticed a pattern.
Over the last 1 million years, the earth's climate record has revealed a 100,000-year cycle oscillating between relatively cold and warm conditions, and Sharma's data on the sun's magnetic activity corresponded to the earth's ice age history.
"Surprisingly, it looks like solar activity is varying in longer time spans than we realized," says Sharma. "We knew about the shorter cycles of solar activity, so maybe these are just little cycles within a larger cycle. Even more surprising is the fact that the glacial and interglacial periods on earth during the last 200,000 years appear to be strongly linked to solar activity."
Sharma's calculations suggest that when the sun is magnetically more active, the earth experiences a warmer climate, and vice versa, when the sun is magnetically less active, there is a glacial period. Right now, the earth is in an interglacial period (in between ice ages) that began about 11,000 years ago, and as expected, this is also a time when the estimated solar activity appears to be high.
Beryllium 10 is useful for studying the geology from hundreds of thousands of years ago mainly because it has a half-life of about one and a half million years. In addition, there are two key factors that have affected beryllium 10 production over the last 200,000 years: the earth's magnetic field and the sun's magnetic activity. When there are high-intensity solar magnetic storms, more charged particles are interacting with cosmic rays, and less beryllium 10 is produced. Likewise, the earth's magnetic field changes the flux of cosmic rays into and out of the atmosphere.
Since the production rate of beryllium 10 and earth's magnetic field intensity are known for the last 200,000 years, Sharma could calculate solar magnetic activity for this time period.
"I took sets of existing, independent data and made new comparisons and calculations," says Sharma. Then he went a step further to make a connection with the history of ice ages by looking at oxygen isotopes in the oceans, which reveal the history of how much ice was at the poles and are therefore a measure of average global surface temperature.
"I compared the estimated past variations in the solar activity with those of the oxygen isotopes in the ocean. Although there is a strong relationship between solar activity and oxygen isotopic variations, it is too early to say exactly what is the mechanism though which the sun is influencing the terrestrial climate."
One explanation of the 100,000-year cycle was offered by the Milankovitch Theory of Ice Ages in the 1940s, which suggested that the cyclical variations in the earth's orbit around the sun result in the earth receiving varying amounts of solar radiation that, in turn, control the climate. This explanation is under dispute because the variations of the solar energy in relation to the changes in orbit are very small. Other current research focuses on past variations in the sun's irradiance, or heat intensity (as opposed to the magnetic activity).
Sharma notes that more analysis is needed to test his theory. "I've only looked at 200,000 years. My calculations need to be verified for a million years, for instance. Plus, regarding the current global warming debate, it still needs to be examined if the role of solar activity will exacerbate the rising temperatures that result from carbon dioxide buildup in the atmosphere."
This work was supported by Dartmouth College, the Max Planck Institute and by a grant from the National Science Foundation.
Sime, et al.16 have found that past interglacial climates were much warmer than previously thought. Their analysis of the data shows that the maximum interglacial temperatures over the past 340 kyr were between 6 oC and 10 oC above present day values. From Fig. 1, it can be seen that past interglacial carbon dioxide concentrations were not higher than that of the current interglacial, and therefore carbon dioxide could not have been responsible for this warming. In fact, the concentration of carbon dioxide that would be needed to produce a 6-10 oC rise in temperature above present day values exceeds the maximum (1000 p.p.m.v.) for the range of validity of the usual formula [∆F=α ln(C/C0)] used to calculate the forcing in response to such an increase.
It is generally understood that the variation in galactic cosmic ray flux is due to changes in the solar wind associated with solar activity. The sun emits electromagnetic radiation and energetic particles known as the solar wind. A rise in solar activity—as measured by the sun spot cycle—affects the solar wind and the inter-planetary magnetic field by driving matter and magnetic flux trapped in the plasma of the local interplanetary medium outward, thereby creating what is called the heliosphere and partially shielding this volume, which includes the earth, from galactic cosmic rays—a term used to distinguish them from solar cosmic rays, which have much less energy.
When solar activity decreases, with a consequent small decrease in irradiance, the number of galactic cosmic rays entering the earth’s atmosphere increases as does the amount of low cloud cover. This increase in cloud cover results in an increase in the earth’s albedo, thereby lowering the average temperature. The sun’s 11 year cycle is therefore not only associated with small changes in irradiance, but also with changes in the solar wind, which in turn affect cloud cover by modulating the cosmic ray flux. This, it is argued, constitutes a strong positive feedback needed to explain the significant impact of small changes in solar activity on climate. Long-term changes in cloud albedo would be associated with long-term changes in the intensity of galactic cosmic rays.
Earth’s protective magnetic field has been weakening at a faster rate than expected, according to data from newly launched European Space Agency satellites. The finding may indicate that Earth’s poles will switch sooner than scientists thought.
It was previously thought that the field was weakening by about 5 percent each century, LiveScience reports, pointing to a flip in about 2,000 years. But the new data shows a much more dramatic weakening, at a pace of 5 percent per decade — 10 times faster than previously thought.
The new data come from a trio of satellites collectively known as Swarm, launched by the ESA in November. The measurements show a dramatic weakening over the Western hemisphere, with some strengthening in other areas, like the southern Indian Ocean, according to a release.
So for some reason this means that CO2 is not causing the current warming?
From Fig. 1, it can be seen that past interglacial carbon dioxide concentrations were not higher than that of the current interglacial, and therefore carbon dioxide could not have been responsible for this warming.
Sharma notes that more analysis is needed to test his theory. "I've only looked at 200,000 years. My calculations need to be verified for a million years, for instance. Plus, regarding the current global warming debate, it still needs to be examined if the role of solar activity will exacerbate the rising temperatures that result from carbon dioxide buildup in the atmosphere."
Another uncredited quote from you. The trouble is there has been a decline in solar activity since 1950 which means temperatures should have fallen, right? They didn't.
When solar activity decreases, with a consequent small decrease in irradiance, the number of galactic cosmic rays entering the earth’s atmosphere increases as does the amount of low cloud cover. This increase in cloud cover results in an increase in the earth’s albedo, thereby lowering the average temperature.
I thought you were comparing the medieval warming period to the current climate. As you point out the slowing of the North Atlantic current (which could be well be due to a growing influx of fresh meltwater) could result in cooler regional temperatures.
Secondly...you say that there have been no changes in ocean currents. Except that the NOAA has shown measurable slowing in the North Atlantic current. This may be responsible for the recent growth in the arctic ice cap.
As mentioned before, globally melting glaciers, coupled with rising ocean temperatures, could have catastrophic impacts on oceanic circulation in the future. Thermohaline Circulation mixes temperature and salinity, and regulates the density of ocean water.
Another uncredited quote from you. The trouble is there has been a decline in solar activity since 1950 which means temperatures should have fallen, right? They didn't.