Can we see satellites at night?

Yes, we can see satellites in particular orbits as they pass overhead at night. Viewing is best away from city lights and in cloud-free skies. The satellite will look like a star steadily moving across the sky for a few minutes.

If the lights are blinking, you probably are seeing a plane, not a satellite.

Satellites do not have their own lights that make them visible. What you will see is sunlight being reflected off the satellite, often off the large solar arrays that provide power to the satellites.

These satellites are very high above Earth, about 200 to 300 miles so, while you are in the night darkness, the satellite can still be illuminated by the sun.

Eventually the satellite will fly into the Earth’s shadow and then suddenly disappear from view.

The International Space Station (ISS) can be very bright.

It orbits Earth at an altitude of about 215 miles traveling at a speed of 17,200 mph.

It is a large object with large, highly reflective solar panels making it the brightest of human objects orbiting Earth. It can be as bright as Venus.

You can find out when the ISS is flying over you by visiting the website go.madison.com/space-station and entering your state and city, or selecting one of the nearby cities from a list.

Weather satellites that track clouds and whose images are shown in animations on many websites are orbiting 22,000 miles above us and appear fixed over the equator.

You will not be able to see those moving across the sky.

Category: Meteorology

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Is the recent Alaska heat wave setting us (Madison, WI) up for a warm late June?

We have not been subjected to extreme heat this summer. In fact, through June 18, we are about 0.2 degrees below normal for the month. That appears to be about to change as a massive ridge of high pressure will be in place over the central United States by the time you read this.

We suspect that will mean our first few days of temperatures over 90 degrees during this week. Interestingly, the circumstances leading to this rather usual onset of summertime heat may be pretty unusual.

It appears that an incredible heat wave in Alaska last week (June 16-19) may have set the stage for our coming warm week. The towns of McGrath and Valdez, Alaska, were both over 90 degrees last week (20 and 17 degrees above normal, respectively). There were numerous other reports of temperatures over 90 in Alaska last week — the highest being 96 near Denali National Park.

Valdez had an overnight low of only 69 on June 17.

All of this unusually warm Alaska weather was associated with an incredibly unusual ridge of high pressure at about three miles above the ground. Such a feature keeps the skies clear and, coupled with the very long days in central Alaska near the summer solstice and flow down the sides of the high mountains, the temperatures were able to soar. The evolution of the Alaskan ridge is the main connection between last week’s heat in Alaska and our heat this week.

Category: Meteorology

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How’s the hurricane season looking?

Hurricane season runs from June 1 through Nov. 30. The National Oceanic and Atmospheric Administration has been making seasonal forecasts for about the last decade. Their Atlantic Hurricane Season Outlook for this year indicates there is a 70 percent likelihood of having 13 to 20 named storms, of which seven to 11 could become hurricanes, including three to six major hurricanes.

If a tropical storm has wind speeds that are 39 mph or higher, the storm gets a name. It becomes a hurricane if it has winds of 74 mph or higher, and a major hurricane if it has winds of 111 mph or up.

In an average season, the Atlantic Ocean sees 12 named storms, six hurricanes and three major hurricanes. So, if the forecast holds up, we are in for an active hurricane season.

The forecast is based on current and expected conditions. First, an active season would be predicted if the sea surface temperatures are warmer than normal. Warmer temperatures increase evaporation off the sea surface, and that provides the energy for the storm. The forecast is also a function of the El Niño conditions in the Pacific Ocean.

On average, El Niño years are low-hurricane years as during such years a strong jet stream exists over the subtropics. That can destroy the carefully organized circulation of hurricanes.

Perhaps surprisingly, the atmospheric pressure pattern over the Arctic also plays a role in the forecast: High pressure means a weaker jet stream, which favors hurricane development.

Category: Tropical
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Can we predict the kinds of tornadoes that hit Oklahoma?

Through the end of last week, this spring had been well behind the average in number of reported tornadoes in the United States. Though we are still running a lower than average year, the recent devastation in Moore, Okla., has brought tornadoes back into the news in a dramatic way.

Why we have been below normal so far is a question prompting ongoing research and may be addressed in a future column.

The Moore tornado was rated an EF5, the strongest tornadic storm, with estimated wind speeds in excess of 200 mph near the core. The other alarming characteristic of the Moore tornado was its exceptional size (over 11/2 miles wide) and the fact that it stayed on the ground for so long (over 40 minutes).

Though we understand the general conditions under which tornadoes are likely to develop, the exact details of tornado formation are still not well known. This makes precise prediction of these storms a near impossibility.

In order to protect the public as best it can in the face of this difficulty, the National Weather Service employs a network of trained tornado spotters along with Doppler Radar data to identify tornadoes as soon as they develop.

In fact, since the Barneveld tornado of June 1984, the average warning time for tornadoes has risen from just under 5 minutes to nearly 15 minutes.

Though not a replacement for point-specific forecasts of tornado occurrence, the combination of vigilance in the face of high likelihood and rapid public alert systems has saved many lives in the past 20 years and probably saved dozens, if not hundreds, of lives last week in Moore.

Category: Severe Weather
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What were those lumpy-looking clouds over Madison last Tuesday

Mammatus Clouds

Mammatus Clouds • Dave Jones, UW-Space Science and Engineering Center

Those types of cloud are called mammatus. They often extend from the bottom of the anvil cloud of a thunderstorm, also called a cumulonimbus cloud, and indicate an intense storm is nearby. This was the case on Tuesday. Mammatus clouds may have a very ominous appearance; however, they are usually seen after the worst weather has passed. When they occur near sunset, they provide a beautiful sky.

Mammatus occur frequently in the Midwest during summer. We do not fully understand why they form, but there are a few hypotheses for their occurrence. Unlike most clouds, which form in rising air, mammatus are associated with sinking air in the upper parts of a thunderstorm. We also know that to form, there must be rapid changes in temperature, moisture and wind between the bottom of the anvil and the cloud-free air below. This rapid change in wind is a hazard to aviation, so pilots avoid mammatus and thunderstorms in general.

The widely accepted cloud classification system used today is based on a scheme introduced by Luke Howard in 1803. This naming convention uses Latin roots to describe the appearance of different cloud types. The Latin ‘mamma’ means udder or breast, and refers to the clouds’ characteristic udder-shaped protuberances.

Rooftop Video

Rooftop Video

Check out this video to see the storm from the rooftop cameras atop the AOSS Building.

Category: Phenomena

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