Some comets are bright enough for the cone cells in our eyes to detect their color, which can reveal whether the comet is richer in gas or dust. Yellow implies dust, while blue implies gas. Some comets also display green heads, a result of ultraviolet radiation breaking down diatomic carbon molecules (C2 ), causing the head, and only the head, to fluoresce. The tails of dusty comets usually shine with a white or pale-yellow light, like straw under a setting Sun. When bright dust tails are seen close to the horizon, they can also take on a reddish hue due to dust or other contaminants in Earth’s atmosphere, making them appear like bloody swords.
Ion tails, meanwhile, require greater effort to observe. They consist of electrically charged, glowing molecules, or ions, that follow the path of the solar wind almost exactly. The most common ion, CO+ (carbon monoxide), absorbs sunlight and fluoresces at a wavelength of 420 nanometers, so ion tails tend to appear blue. Some observers, especially those with eyesight particularly sensitive to blue light, can see them clearly. English astronomer George Alcock was renowned for his observations of comet ion tails. Most observers, however, must work a bit to see them, especially when faint.
If an ion tail is present, use averted vision and sweep your telescope back and forth across the area of the sky behind the comet’s head in the anti-solar direction. The same method can be used for naked-eye comets with a long ion tail — only in this case, sweep your eyes back and forth across the sky. The latter is the same technique an observer would use to bring out the zodiacal light against the background sky.
If a gaseous comet passes close to Earth, it can be an awe-inspiring sight. Such was the case with C/1996 B2 (Hyakutake), which came within 9.3 million miles (15 million kilometers) of Earth, or about 40 times the Earth-Moon distance. At its closest, Hyakutake’s head swelled to greater than four Full Moon diameters, while its tail stretched more than halfway across the sky like a banner of pale light.
Ion tails often display hairlike streamers or braided (ropey) flows of gas. These tails can also appear frayed, with structures branching off from the main tail. Among the most remarkable phenomena associated with ion tails, however, is a disconnection event. These are triggered either by debris violently ejected from the comet’s surface or by coronal mass ejections from the Sun slamming into the comet. Disconnection events occur when strong fluctuations in the solar wind pinch the magnetic field lines in the ion tail together, forming a knot that releases a powerful burst of energy strong enough to sever the tail, causing it to drift away. In some bright comets, knots and the resulting disconnection events can be observed with unaided eyes.
Finally, very rarely, comets can display anti-tails (type III) that appear when Earth passes through or close to the plane of a comet’s orbit around the Sun. When this occurs, we see dust in the comet’s orbit edge-on, causing it to appear like a sunward-pointing tail that lags behind the comet. Because anti-tails reflect sunlight, they are not difficult to see. Look for a long, slender lance (sometimes surrounded by an ellipsoidal envelope) or a triangular wedge fanning out from the comet’s head. What we see depends on our viewing angle: The more needlelike the anti-tail, the closer Earth is to the comet’s orbital plane.
Whatever tails are visible during your next observing session, you can determine their lengths and position angles by recording the positions of the comet’s head and tail against the background stars, then plotting them on a star chart. Next, measure the length of the tail (usually in arcminutes or degrees) from where it comes off the comet’s head to its tip. To determine position angle, use a protractor to measure the tail’s orientation relative to the center of the coma, with north at 0°/360°, east at 90°, south at 180°, and west at 270°. For comets with broad dust tails, measure the two endpoints of the tail’s width and record the extent; for example, a dust tail may sweep across the sky from a position angle of 45° to 90°.