An evening after the rain at the Station de la plage, Québec 2024
A few Quebec City residents enjoy the last glimmers of daylight at the Station de la Plage, as the showers of the previous hour precipitated the departure of the other occupants.
Radar echoes showed towering cumulus clouds (TCU) approaching the area at around 19:00. These usually produce short-lived showers, letting light through here and there between the cloud formations.
For a photographer, the first ingredient in capturing a special sky is present.
The second prerequisite is that the setting sun’s rays travel a greater distance through the atmosphere, unblocked by a distant weather system. This makes it possible to observe such impressive shades of pink and red. So, we check the forecast to verify that this is no weather system coming the next day.
These two conditions greatly increase the chances of an interesting sky at dusk. It doesn’t always work, but let’s just say that planning improves the likelihood of a successful photo shoot.
That’s what happened on this August evening in 2024.
Evening sky visible through the installations at the Station de la plage, Québec 2024
The photo above shows the shades of sky visible through the openwork ceiling of the Station de la plage. I like the minimalist look. It vaguely reminds me of the paintings of Canadian NewfoundlanderChristopher Pratt. For him, the primary interest lies less in the representation of an architectural structure as such than in the addition of light that will transform the viewer’s perception.
Sea kayaks at Saint-Laurent-de-l’Île d’Orléans 2023
On Sunday, September 24, 2023, the company Quatre Natures organized a certified level 1 sea kayaking course the St. Lawrence River, starting from Île d’Orléans. As registration was done well in advance, we had to be a bit lucky during the activity, as it would take place as much in good weather as in bad.
So, I take a chance. Fortunately, an incredible day awaits the six students: full sun and twenty degrees Celsius. How should we dress for the circumstances? We know that the human body temperature is 37 degrees Celsius. The kayaker adds up the water and air temperatures and compares the total to the temperature of the human body. With the river that day at 18 degrees and the air around 20 degrees, this gives a total of 38. As this figure is slightly higher than normal body temperature, we can wear normal clothing for water activities, rather than a wetsuit.
The morning is used to cover theory. No one sets foot in the water. The instructor discusses what the kayaker must have on board, the relative quality of different equipment, preparation, communications and radio frequencies, safety and hypothermia prevention, and so on.
Sea kayaking activity at l’île d’Orléans (photo Vadym Kravchenko)
After lunch, the kayaks are placed on the lawn and the vocabulary related to each part of the kayak is learned. The student then settles into the kayak and learns how to adjust the footbraces, hold the paddle, install the spray skirt, and so on. The boats are then brought to shore and kayaking begins.
First, we learn the basic maneuvers. How to embark and disembark, the trajectory the paddle should follow in the water depending on whether you want to go forward, backward or turn. We discuss the correct position of the body, arms and wrists on the paddle, and the importance of rotating the pelvis to force the paddle properly. We quickly realize the influence of side winds on the kayak, especially when it has no centerboard or rudder.
The river is considered level 2 for kayaking. The current is strong, and we have to deal with three-metre tides. The wind around the island is also stronger than in Quebec City. Level 1 kayakers are encouraged to seek out Level 1 locations to gain experience, and never to set off alone at this stage of their learning process.
During the exercises, you can see the container ships and the various pleasure boats offshore. The larger vessels generate waves that take between five and ten minutes to reach the shore. When these approach, the instructor warns novice kayakers to turn to face the wave, so as to limit the effects on the boat.
The container ship Hapag_Lloyd Quebec Express and the container ship MSC Paola are sailing around Île d’Orléans near Quebec City.
The BBC Manila carries wind turbine blades on the St.Lawrence Seaway near Quebec City.
Then come the emergency maneuvers: what’s the procedure for getting out of a kayak that’s just capsized? How do you help someone who has capsized?
I didn’t have time to get to this stage of the course. I capsized before. I don’t remember how I managed to extricate myself from the kayak and get back to the surface, but we’re not talking about an approved method here. The brain immediately detects the danger and organizes itself so that the body gets out of the kayak and the head doesn’t stay underwater for too long.
In the minutes that follow, the instructor teaches us how to perform the classic exit from a capsized kayak. We work in pairs. At Level 1, there’s no question of using the paddle to force the kayak to turn.
To obtain KDM 1 certification, everyone must lean sideways so that the kayak tips over. Once submerged, the student leans forward, unhooks the spray skirt attached to the kayak, and slowly taps the kayak’s hull three times to signal that he is in control of what he is doing. The instructor wants to avoid unpredictable reactions. We then push ourself out of the kayak by placing our hands at hip height on the coaming. As soon as we are out of the water, it’s imperative that we hold on to our kayak, thanks to the lifeline. It only takes a few seconds. Here and there, you can hear a little coughing as the student surfaces, but nothing more. A good sip of St. Lawrence River boosts the immune system.
Next comes the recovery of the person in the water. As we work as a team, the kayaker in difficulty clings to the front of our kayak and stays there until we catch up with his or her kayak, lift it onto our boat, empty it of water, turn it over and position it correctly.
Sea kayaking course level 1 with Quatre Natures (photo Quatre Natures)
The person clinging to the kayak then releases his or her grip, and depending on the method taught, climbs back into the boat while the latter is being held securely. The important thing here is to keep the center of gravity as low as possible. If the person doesn’t hurry and proceed step by step, the operation is a success every time.
A few more exercises follow, and it’s back to the beach on Île d’Orléans a few hours later. Once all participants have dried off and put on their warm clothes, the course concludes with a few weather notions, including the need to consult weather forecasts and radars, and to return quickly to shore when storm cells are present.
We also cover tide calculation (rule of 12) and how to attach a kayak to a car roof. How many attachment points? What equipment is available to make the job easier? Where should harnesses go to avoid breaking the kayak? Etc.
The KDM 1 certificate is awarded approximately eight to nine hours after the start of the course, depending on the instructor’s assessment. I noticed that on the way home, in the heat of the car, I really didn’t feel like rushing on the road. But you quickly come back to reality when you see how fast the cars are coming up behind you.
A roll arcus cloud in development ahead of a thunderstorm approaching the Quebec Jean-Lesage airport in 2012.
Summer 2012. A very active cold front had been sweeping across the province and was about to hit the Québec Jean-Lesage international airport (CYQB). Considering the winds and the temperature spread, as well as the weather radar, it was obvious that it would be a very interesting show.
The Nav Canada control tower and flight information center (FIC) being collocated, the common stairway surrounding the tower became a privileged spot from where to take pictures. As a flight service specialist (FSS) on a short morning break, I grabbed my camera and headed outside on the stairway, just in time to see a line of roll arcus clouds arrive over the mountains to the north-west.
A roll arcus cloud ahead of a thunderstorm heading for Quebec City in 2012
The first showers started, quickly followed by strong gusty winds and hail. In order to protect myself from the severe weather, I just had to slightly change position on the stairway and use the tower as a shield. Satisfied with my shots, I abandoned my observation post and let Mother Nature express herself.
A roll arcus cloud in development ahead of a thunderstorm approaching the Quebec Jean-Lesage airport in 2012.
An arcus cloud ahead of a thunderstorm approaching the Quebec Jean-Lesage airport in 2012
An arcus roll cloud in delopment near the Quebec Jean-Lesage airport in 2012
Nav Canada control tower with, in the foreground, several CL-215 and Cl-415, a Nav Canada Challenger, and an Air Transat Airbus at the Quebec Jean-Lesage international airport (CYQB).
On a stormy summer day, Air Canada called the Nav Canada flight information center (FIC) at the Quebec Jean-Lesage international airport (CYQB) on the Montreal frequency. The pilot was flying an Airbus and was about to take-off from the Montreal Pierre-Elliott-Trudeau international airport to Halifax, but there was violent weather that had to be avoided.
Normally, big airlines have their own briefing and flight planning services. However, rapidly changing weather sometimes requires last minute adjustments. In the case of the Air Canada flight, severe thunderstorms forbid a direct path from Montreal to Halifax. The pilot was looking for the best option: go around the thunderstorms by flying north over Mont-Joli then eastward to Halifax or fly southward to United States then head east to Halifax.
Both solutions were possible but the objective was to pick the route that would diminish the pilot’s chances to have to divert to an alternate airport.
Radar imagery became the essential tool to propose a solution. Knowing the time lapse between two images, it was possible to evaluate the weather system’s speed. By calculating what was the distance left for the system to arrive in Halifax, and knowing the system’s speed, the flight service specialist (FSS) was able to estimate as precisely as possible the time when the thunderstorms would move over the destination airport.
The pilot having calculated the estimated time of arrival to Halifax for both the south and north routes, and now knowing at what time the weather system would be over Halifax, he understood that the best option was the southern route through United States. If there was no last minute modification in the system’s speed, he would be able to land in Halifax between twenty and thirty minutes before the first thunderstorm cells arrive over the airport.
It is fairly uncommon to receive an official feedback from the pilot of a big company like Air Canada. But the next day, surprising the flight service specialist (FSS), the pilot called back, presenting himself as the one who had made a flight from Montreal to Halifax the precedent day. He wanted to thank the FSS who had helped him in his decision making since, as he said it, the route via the United States had been a success and he was able to land his Airbus thirty minutes before the arrival of the thunderstorms. That kind of call certainly helps any employee to start a working day on the good foot…!
Old Quebec airport terminal with an Air Canada DC-9 and a QuebecAir BAC 1-11 (on aviation postcard)
Around 1996, during the summer, an Air Canada DC-9 captain visited the Transport Canada flight service station in Québec City (CYQB) to receive a last minute briefing on the weather conditions between Quebec and Toronto.
All the passengers were already on board, but the captain had noticed a rapid change in the size of thunderstorms approaching the Québec City airport. Wishing to make the best decision, he requested the latest information on the approaching line of thunderstorms before proceeding with the takeoff.
The weather radar and satellite pictures showed a wall of convective cells that a DC-9 would not be able to go through. It would not fly high enough nor be able to go around the system unless it made a detour through Val-d’Or to the north or the Tennessee to the south.
The captain already knew the consequences of his decision. He nonetheless took the phone and called Air Canada’s dispatch in Toronto, announcing that he would not leave Quebec until the weather was acceptable. He could envision the missed transfers in Toronto for most of his passengers, and their bad mood in face of the lengthy delays he expected in Québec City.
Nevertheless, his decision was made and he left the flight service station satisfied. He knew very well that a line of heavy thunderstorms had often been the cause of accidents and that no aircraft, whatever the size, was safe when dealing with a wall of severe thunderstorms.
The flight service specialists (FSS) were happy with the captain’s decision since, throughout the years, the FSS often witnessed far less commendable behaviour from pilots of all categories. Judgment is the capacity to evaluate consequences, and it is not given to everybody.
1986. It was a beautiful summer afternoon at the Rouyn-Noranda airport (CYUY). The Transport Canada flight service station employees knew that a cold front was approaching and would soon sweep the airport. Until then, it was still a perfect day. Blue sky, light winds. At the time, the flight service specialists (FSS) did not have access to radar images or satellite pictures.
To get an idea of what was coming from the west, we were normally using an Environment Canada aviation weather forecast and the actual weather observations of two flight service stations in Ontario, Earlton FSS and Timmins FSS. Their last weather observation mentioned a wind shift and an isolated thunderstorm. But Timmins was far away and could only provide us with a rough estimate of the situation.
As I was working the evening shift on that day, I checked the wind speed indicator, as a reflex developed throughout the years. What I saw was kind of unreal. The speed indicator’s needle suddenly went from showing few knots to 20 knots, and then 40 knots, hesitated a little then went up to 60 knots and, in a final correction, reached 72 knots, which was about 134 km/h.
Everything was so peaceful around the flight service station. I looked through the window to detect any moving object. At that very moment, the wooden shed normally used by the fuel man passed in front of the station. That wooden structure must certainly have weighted few hundred kilos. The fact that it was moving at a good speed was a clear indication that the instruments were working properly. A squall line was associated with the cold front progression.
Everything that was not properly fixed to the ground started moving. In the next hour, strong thunderstorms going eastward moved in over Rouyn-Noranda. The Val-d’Or airport (CYVO) being located sixty miles east, it was clear that it would be hit directly in about two hours. I called the Val-d’Or control tower so that everyone got prepared for the squall line. That gave them enough time to tie everything correctly and damages were limited.
One hour later, everything was back to normal in Rouyn-Noranda and we profited from an ideal summer night.
For more real life stories on the Rouyn-Noranda flight service station and flight service specialists, click here:
Cumuliform clouds add energy to any photo. Even photos in black and white benefit from them largely, whether it is for a normal or an HDR photo.
Cumuliform clouds add dynamism to this Abbaye du Mont St-Michel scenery. France (1978)
Black and white HDR picture of lamp posts installed along the St-Lawrence, Quebec City 2012.
The stratiform clouds add to the tranquillity and the stability of a photo.
Daytona Beach under stratus clouds in 2011. The end of the afternoon allows the fresh air from the sea to move over the heated land, which helps create few cumulus fractus, visible near the buildings.
Clouds including a stratiform and cumuliform components (stratocumulus) produce an effect that is more energizing than the simple stratus, while avoiding the explosion of energy of the cumuliform clouds.
A stratocumulus adds to this otherwise peaceful scenery captured on board the Lyria train between Paris and Geneva in 2013.
The cold front
The approach of a cold front enhances the possibility of interesting photos. If it is a fast moving cold front of moist and unstable air, the photos will probably be more spectacular, as some thunderstorms will be associated with the system. A dew point of more than 15 C indicates the presence of a lot of water vapor which can be transformed into precipitation, thus releasing a lot of energy. When these conditions are combined with a really strong contrast between the new air mass which approaches and the one which goes away, the produced meteorological phenomena will certainly be intense.
In the photos below, the meteorological system approaching the Quebec Jean-Lesage international airport also had to cross a small mountain range.
A roll arcus cloud in development ahead of a thunderstorm approaching the Quebec Jean-Lesage airport in 2012.
A roll arcus cloud in development ahead of a thunderstorm approaching the Quebec Jean-Lesage airport in 2012.
View under a developing arcus cloud at the Quebec Jean-Lesage international airport (2012)
An arcus cloud ahead of a thunderstorm approaching the Quebec Jean-Lesage airport in 2012
A roll arcus cloud ahead of a thunderstorm heading for Quebec City in 2012
The morning fog
The morning fog offers many opportunities for interesting photos. You can choose an isolated tree and capture the combined effects of the morning sun and fog. Or you may choose a cluster of trees, for a completely different effect. Both photos below were taken in Domaine Cataraqui, Quebec City.
Trees in fog at Domaine Cataraqui, Quebec City 2009
Sun and fog provide for a special atmosphere at the Domaine Cataraqui, Quebec City 2009
A morning fog resulting from a cold cloudless night will persist for hours if there is no wind. The cold morning air, motionless over a slightly hotter stretch of water, creates a fog that will finally disappear just before noon, when the atmosphere has been heated enough. If there had been an overcast sky during the night, chances are that the air over the water would have remained at a higher temperature, preventing the formation of fog.
The opportunities for more interesting photos arise when you witness the first holes in the fog layer.
The Ocean tugboats during a dense fog in the Bassin Louise in Quebec (2012).
We can take into account the season to estimate the speed of the diurnal reheating of the lower atmosphere. A morning fog will need more time to dissipate from late autumn to early spring: that leaves more time for the photographer to prepare. The forecasts can announce the disappearance of fog while it will not be the case if, over your sector, there is an invading layer of stratocumulus preventing the morning sun from reaching the ground.
To determine if the fog is going to dissipate as expected or will remain and possibly intensify, watch the difference between the temperature and the dew point on the hourly meteorological observations issued by weather stations near your place of residence. If the temperature and dew point spread increases, the fog is going to lift. If the difference between those two decreases, the fog is going to persist and possibly intensify.
The mist
The mist can be qualified as such when the visibility is superior to ½ mile, but do not exceed 6 miles for an observer on the ground. If the visibility is of ½ mile or less, it is called fog. This photo of the Bic National Park, near Rimouski, shows the interesting effect that the mist adds to a beautiful landscape.
Mist in the Bic National Park, Province of Quebec (2009)
Hot and unstable air in winter
When there is a warm and unstable air advection (about 0 degrees) while winter has already settled, there are good opportunities for photos. A moderately developed cumulus produces significant snow showers and this snow sticks on all the surrounding objects. All that snow would have begun to melt on contact of objects if the latter had had a temperature superior to zero degree. But, the winter being already settled, the snow persists. It gives enough time to capture some souvenirs.
A Quebec City street after a snow shower
The local effects
A photographer might benefit from learning about the meteorological local effects influencing the regions he intends to visit. The local effects are often simple to understand and they repeat themselves regularly, according to wind and season changes. The knowledge of these effects allows the photographer to be ready and position himself even before the phenomenon occurs. It limits the comments like: “If I had known that it would occur, I would have settled down here one hour earlier!“
The local terrain as well as large size bodies of water produce predictable meteorological phenomenon that can be used by a well prepared photographer. It can consist of persistent fog, repetitive snowstorms over a small sector, strong winds, cumuliform clouds alongside the mountain summits, etc. By being positioned at the right place, at the right time, the desired photo can be realized.
A change in the wind direction
A change in the wind direction suddenly increases the opportunities of interesting photos. It might announce the approach of a cold front, a warm front, a sea or land breeze, etc. In the photo below, a bit of fresher air suddenly began crossing the St-Lawrence seaway at the end of the day, thanks to the approach of a weak cold front. The water was still relatively warm and the moisture which was present over the surface became visible due to the cool air supply. The conditions were now ideal for a short-term thin fog, as long as the wind speed would not increase. Just in time for a photo.
The new wood pellets silos in Anse au Foulon in Quebec City en 2014
Familiarization with weather radars
It can be useful to get acquainted with weather radars which, for the needs of photography, remain simple to interpret. Multiple echoes of small dimension with a steep gradient of various colors indicate precipitation resulting from cumuliform clouds. The showers associated with these clouds are often moderated or strong and will be the result of approaching towering cumulus or cumulonimbus (thunderstorms). A towering cumulus presents a dark base and a white summit to the photographer. At sunset, their vertical development can be used to emphasize the last rays of light.
The side of a towering cumulus (TCU) is benefiting from the remaining sunlight over Quebec
Large echo areas of similar colors of low intensity indicate a relatively stable air generally producing steady light rain or drizzle. This should be understood as a possibility of increased humidity limiting the visibility through mist or fog.
Hoar frost
Hoar frost is a short-term phenomenon. It is thus necessary to capture the scene before the sun melts everything. The photo below shows some small twigs on which hoar frost has settled. It was taken at the beginning of the seventies. Although the quality of the photo is not exceptional, the meteorological phenomenon is well demonstrated.
A combination of snow and hoar frost observed on a Quebec field in 1976.
Forest fires
Wishing to make photos of western Canada during summer 2014, I came up against a season where hundreds of forest fires were raging. The smoke was covering some parts of Alberta and British Columbia. Some fires were important enough to require the closure of the sole highway connecting Lake Louise to Jasper. I thus decided to include the effects of those fires in the holiday souvenirs.
A visibility reduced in forest fire smoke allows a photographer to obtain, without special editing, sunsets with interesting colors.
Sunset and smoke from forest fires in Kamloops in 2014
The smoke also produces an effect similar as fog, but a fog which would be impossible to obtain at the end of a summer afternoon while the sun shines and there is a 38 degrees Celsius temperature.
An area near Kamloops, Canada, that was touched by forest fires in 2014
At dusk, the residual smoke is visible near tree tops while the setting sun strikes the mountain side. The effect is of two horizontal lines of complementary colors, blue and orange.
Forest fire smoke and sunset combined in Lake Louise, Alberta en 2014
(Precedent story: the commercial pilot license / a tire bursts on landing)
On a hot summer day of 1981, I was asked to fly a Cessna 150 to the Montreal Pierre-Elliott-Trudeau international airport to pick-up one of our flight instructors and bring him back to St-Jean-sur-Richelieu. The winds were blowing from the northwest, so runway 28 was being used. While I was in final for that runway, the air traffic controller realized that he did not have enough separation between my plane and a heavy one that was also in long final. He told me “Increase your speed, there is a Boeing 727 behind you”.
It is very easy to increase the speed of an airplane while maintaining an altitude. You just push the throttle and the speed increases. However, when the aircraft is above the threshold of the runway, it needs its specific speed to touch the ground otherwise it continues to fly until the appropriate speed for landing is reached. It seemed to me that the Cessna floated for an eternity before finally touching the runway. But it eventually worked out well and I exited the runway before an overshoot was required for the Boeing.
So I parked the aircraft near Transport Canada’s offices and waited for the instructor for about thirty minutes. Clouds were rapidly covering the sky in this late afternoon, with all the humidity and an already high temperature. When the instructor finally showed up and we proceeded with the taxiing procedure, the air traffic controller told us: “You must accept radar vectors for your departing route because of the weather.” What weather? A cold front was at work, but nothing serious was visible from our position. So close to the airport terminal, all we could see were towering cumulus, nothing else. We accepted his offer in order to be allowed to leave the airport.
The take-off was made from runway 28. I made a left turn toward St-Jean. We soon understood why radar vectors had to be followed. A storm had developed between Montreal and St-Jean. We observed what looked like five cylinders created by heavy rain. Lightning was also occasionally visible. We had to fly between the cylinders to avoid the most problematic areas. We tightened our seat belts just as the first bumps were being felt, making our altitude vary considerably. Knowing what I know today about flying in bad weather, I would not attempt another flight like this one, especially without an onboard weather radar.
The flight ended nicely with a smooth landing in St- Jean, outside of the problematic weather area. A few weeks later, I was asked if I would accept to be captain for a long flight across Canada. This unexpected offer represented a great opportunity, especially since it would allow me to log more than forty additional flying hours.
(Next story: a visual flight (VFR) from St-Jean-sur-Richelieu, Quebec, to Emonton, Alberta)
