Wednesday, July 28, 2010

Can the Phases of the Moon Affect Precipitation?

Often dismissed as an old superstition, but does the changing phases of the Moon affect when it would rain or snow?


By: Ringo Bones


I don’t know how many heard of it, but I first heard this supposedly old superstition back in 1989 that goes: Wet weather follows the new Moon and the full Moon. Dry weather follows the first quarter Moon and the last quarter Moon. Strangely enough, a correlation was indeed found out at that time using U.S. Weather Bureau precipitation records showing that there is indeed a better than average chance of rain or snow in the week after a full Moon and the week after new Moon. While the driest periods tend to occur the week after the first quarter Moon and the week after the last quarter Moon. Unfortunately at the time, no clear-cut explanation was provided behind the phenomena after the study was published showing a correlation between occurrence of precipitation and the phases of the Moon. Will a renewed study ever shed light on the validity of this old superstition?

My hypothesis on the matter is that probably during the week after the full Moon and the week after the new Moon, the gravitational effects between the Earth and the Moon during these periods probably allowed higher than average amounts of meteoric and cometary dust to fall into our atmosphere. These comet and meteorite sourced material probably acted as nuclei via the Bergeron-Findeisen Theory of Rain / Precipitation thus causing rainfall and snowfall frequency to increase a week after the full Moon and the new Moon. But is this explanation really satisfactory?

Swedish meteorologist Tor Bergeron first proposed the nuclei theory of precipitation around the mid-1930s, which was later elaborated by German physicist Walter Findeisen and is now widely accepted as the Bergeron-Findeisen Theory Rain. This theory was later applied as the working principle behind cloud seeding. Artificial seeding of rain clouds to induce precipitation during times of drought was developed in 1946 by General Electric’s Vincent J. Schaefer and Irving Langmuir. They used both silver iodide and dry ice as cloud seeding material.

Silver iodide, whose crystalline structure is similar to that of natural ice and therefore provides hospitable nuclei on which ice crystals readily form. Solid carbon dioxide or dry ice – another good cloud seeding agent - is so cold that it causes water vapor to solidify into enormous numbers of tiny ice crystals. In either case, precipitation should follow, according to the Bergeron-Findeisen Theory. Pellets of dry ice are usually sown into a cloud from airplanes while silver iodide is released as smoke, sometimes from an airplane, sometimes from the ground. Meteoric and cometary dust could act as a cloud seeding nuclei, increasing chances of rain or snow – depending on the season – during the week after full Moon and the week after new Moon.

Monday, July 19, 2010

Johannes Hevelius: Father of Selenology?

Given the existing technology at the time, did Johannes Hevelius (1611-1687) able to know more about the Moon in comparison to his astronomy contemporaries?


By: Ringo Bones


Some astronomers think that we only managed to know more about the Moon than Johannes Hevelius did when we had the ability to send robotic spacecraft and manned exploration of the Moon, but is there some truth to this? Even though it was Galileo who first documented the Moon’s topography as seen from his first telescope back in 1610. It was Johannes Hevelius, a notable Polish astronomer born in January 28, 1611 that from his crowded rooftop in Danzig laden with his custom built telescopes – where he gained the fame as the pioneer of Lunar topography a few years later. Hevelius also studied distant celestial objects, but learned little because of dust and other disturbances in the atmosphere over Poland despite using an aerial telescope of his own design that’s 150 feet (46-meter) long – equal to the height of a modern 12-story building.

In collaboration with his wife Elizabeth, they charted the Lunar landscape then published their descriptions in Selenographia back in 1647. During his extensive studies of the Moon, Hevelius got curious of the fact that 59% of the Moon’s surface visible from Earth. During his time, the period between new Moons was already measured with a fair degree of accuracy. And the fact that the same face is always turned toward the Earth with only minor wobbling – the extra 9% of the Moon’s surface seen from Earth – was noted although not explained. The modern explanation is in part that the Moon is not a perfectly symmetrical spheroid. The Moon has a massive bulge, which the Earth’s gravitation attracts like a plumb bob, thus keeping the same hemisphere towards the Earth. With such detailed observations of the Moon, Johannes Hevelus’ contribution to modern selenology was indeed indispensable.

During his lifetime, Johannes Hevelius was also credited for discovering four comets and was noted for his suggestion that the comets revolved around the Sun in a parabola. And his observations on comets were published in Prodromus Commeticus in 1665 and Cometographia in 1688. Hevelius also listed 1,564 stars and in 1661 became the second person on Earth to witness the transit of Mercury – i.e. the planet Mercury moving across the face of the Sun as seen from Earth. Coincidentally, he passed away during his birthday on 1687.