Weather

The most immediate change that meteorologists and pilots see in the weather pattern is an increase in the tropospheric flow across the United States and southern Canada at all levels. This starts in earnest in September and continues through October. Temperatures decrease rapidly in the polar regions as fall progresses, dramatically strengthening temperature contrasts between high latitudes and the tropics. This enhances the jet stream pattern and surface patterns alike. So across the board we see an increase in clear air and mechanical turbulence everywhere.

Checklists get taken for granted-settle into your seat in the cockpit, pull out the booklet or laminated cards, turn to the Before Engine Start page and start following the steps. Fire up the engine(s) and proceed down to After Engine Start and Before Taxi. Sound familiar? For most flying under 14 CFR Part 91, this read-then-do routine is the norm all the way to Parking and Securing. While many pilots with a fair amount of experience-particularly those with their own aircraft-will often go a step beyond and make their own checklists, there are far more efficient methods to get things done on time and in the proper order.

Some users of the National Airspace System live by Standard Operating Procedures (SOPs), and some do not. This is arguably the most significant difference between air carriers and general aviation when it comes to training, testing, and cockpit cultures. This is also, by some measures, a factor in accounting for the differences in accident rates. General aviation, particularly the single-pilot, personal-flying kind, relies not on the use of SOPs, but basic personal minimums for aeronautical decision making.

A cloud is the visible manifestation of liquid water droplets or ice. It forms when humid air cools sufficiently for water vapor to saturate and produce condensation-the dewpoint temperature. On a dry summer day in California, this temperature might be 20 degrees F, and the weather remains clear. On more humid summer days in California, the cloud formation temperature might be 50 degrees, producing morning clouds along mountain peaks. When air is chilled to the dewpoint, the humidity becomes 100 percent and from the texts we expect saturation to occur. But in real life this doesnt always happen. If a given volume of air doesnt contain condensation nuclei-microscopic bits of dust, pollen, etc.-the relative humidity may exceed 100 percent without producing clouds. But for the most part, this relationship between temperature and dewpoint is correct.

Certainly following the airways and the MEAs, and then descending over an initial approach fix or hold would be best. I was just thinking of a case when we werent on an airway, like between Keflavik, Iceland (BIKF) and Narsarsuaq, Greenland (BGBW). We wanted to make sure we were above the OROCA and MSAs for that area when we were descending. I guess we could have stayed at our filed FL170 until over the hold, but given that the airport is at sea level we wanted to start a prudently safe descent beforehand.

Pilots get a pass for confessing to the Aviation Safety Reporting System, while the private sector (Embry-Riddle Aeronautical University), not the U.S. government, maintains one of the largest online repositories of NTSB accident documents. Theres no shortage of lessons to be learned and a great culture of diffusing this hard-won wisdom. So, lets delve into a few randomly selected NTSB accident reports, supplemented by any available press stories.

Both spherics and NEXRAD have blind spots and neither is infallible. Spherics devices can have false negatives because they dont see those static discharges until they happen. While most cells with dangerous opposing currents also produce significant static, nature is inherently unpredictable and the static discharges can lag. Of course, the delays in getting NEXRAD images to the cockpit can lead to significant errors. Plus, radar only seeing precipitation, not turbulence, can cause difficulty interpreting the image.

In the summer of 2014 the FAA published in the Federal Register its intent to do away with the Area Forecast (FA) and replace it with digital and graphical alternatives. The agency wrote that the FA was a broad forecast of limited value and that existing, better, alternatives existed.

A low morning fog crept onto the airport as I cleared a CRJ-900 regional jet for takeoff. The RJ lifted, passing just above the vaporous wall, and I switched him to Departure. I waited, watching for something I dealt with every day as an air traffic controller, but had never witnessed.

Wingtip vortices aren't the only type of disturbed air concerning pilots and controllers. According to the 7110.65's Pilot/Controller Glossary, wake turbulence includes "thrust stream...

My goal in this column is to bring the art and science of forecasting to pilots. This is because forecasts arent perfect and still wont be in the foreseeable future. This is not an indictment of the profession, but an acknowledgement of the realities of the forecast problem. For example, a single balloon launch is used to represent the 400,000 cubic miles of troposphere over Arkansas, and only happens every 12 hours. This is why good forecasters are skeptical of models and blend them with experience, intuition, and their own analysis before making a forecast.

As a pilot you most certainly know that just about everything in aviation has a checklist. We controllers have our own checklists for a multitude of hazardous situations, unauthorized laser illumination included. I pulled up the appropriate checklist while the helo maneuvered.