Rising Waters: Hike with a Scientist in Seaside, OR

Views from Seaside toward Tillamook Head.

A few times a year the tides swell to levels much higher than are typical. These royally high tides are known as King Tides and occur over a few days period, typically in the months of November, December, and January.

With the King Tides, comes a whole host of changes to the coastline—local flooding, potentially increased erosion, and an overall increase in coastal hazard risk. However, King Tides are not necessarily something to run from. Many people flock to the coast to see the King Tides—the crashing waves and high surf are a definitive draw for many wave watchers.

King Tides also offers an opportunity to participate in some community science. Oregon King Tides Project, by the Oregon Coastal Management Program and CoastWatch, ask local Oregonians to snap some pictures of these extremely high tides and post them to their site. The goal of the project is to help coastal communities see their vulnerabilities, especially considering future climate change, so they can better adapt and prepare.

I wanted to learn more about sea level rise on Oregon’s Coast and experience the King Tides. So, I  reached out to Alessandra Burgos of Cascadia CoPes Hub to see if she was open to a coastal ramble.  She agreed.

It was time to head to the beach.

The Hike

  • Trailhead: No Official Trailhead (Start on Avenue U and end at 12th Avenue)
  • Distance: 1.5 miles one way on the pavement; the trail is level.
  • Details: Park on the street or Public Parking at the North End of the Promenade. Public restrooms at North End. The promenade is open to hiking/running and biking. It is a popular spot and can be very busy.

Here Comes the King

It was a mostly sunny winter day during king tides week when Ali (Alessandra) and I met for a walk along the Seaside waterfront. If you want to talk about the ocean, it helps to have a clear view of it as you go.

Immediately, Ali’s dark brown eyes scanned the surf. The waves were coming in fast and there wasn’t much beach left uncovered. The tide was in, way in. 

“I have never been here before,” Ali confessed, “but I would imagine the beach is usually much bigger.”

I tried to imagine what it might look like on a “normal” day. Even having been there, I couldn’t picture it.

“It would be nice to have a before and after,” I confessed.

Before and after picture aside, what we were seeing were king tides—unusually high-water levels at high tide that were expected to continue for the next few days. Begging the question—why?

Ebb and Flow

“What happens with tides is you have the gravitational pull of the moon, which is the strongest force,” Ali explained.

You may have heard that the moon creates tides—and this is mostly true. As the Earth rotates and the moon revolves around the Earth, its gravitational pull causes the ocean to bulge in the direction the moon is facing. This bulge is dragged around the Earth, like a magnet, as it rotates. There is also a bulge opposite the moon due to a lack of gravitational pull by the moon at this alignment.

However, that is not the entire story. As Ali explained: “Then you also have the gravitational pull of the sun, and even though the sun is bigger, it is further away so you don’t get as big a pull.”

However, when the sun, moon, and Earth are in alignment—you get a very high, high tide and a very low, low tide.

“For king tides, everything is in a perfect wonderful alignment,” Ali explained. “The moon is either a full moon or new moon… “ and is in line with the Earth and Sun. This causes a higher gravitational pull on the oceans causing these king tides.

At the time of our hike, it was a new moon. In a couple of days, the king tides would be at their peak. 

“You can see over there it is higher than normal and those wonderful waves rolling in,” Ali pointed out toward the ocean waves again. They were really moving.

The water level at near high tide with waves rolling in.

1 Tide, 2 Tides, 4 Tides, More

“Why do we get two tides here?” I asked next as we sauntered our way down a path to the packed sandy beach.

“That [slightly] has to do with where you are in latitude [because of how the continents are spread out],” Ali responded. “And [mostly] it has to do with the shape of the ocean basin.”

She also reminded me that we have two bulges making their way around the Earth in a 24-hour period, so there are both two high tides, and two corresponding low tides.

If there were no continents there would be 2 equally proportioned high and low tides every lunar day. The land masses block the movement of the tidal bulge resulting in different tidal patterns. On the West coast, we experience mixed semidiurnal tides meaning “You have a high, high tide, low, high tide, low, low tide, and high, low tide… four tides,” Ali listed the different tides, but it came out more like a tongue twister.

We were walking the beach during our high, high tide.

Most places on the Earth experience two tidal cycles. However, there are some places that have only one high tide due to the shape of the ocean basin. The Gulf of Mexico, for example, has diurnal tides, experiencing one high tide and low tide on a lunar day.

A Rough Start

Ali and I headed north along the sandy beach—the waves rolled in a short distance away from us. I asked Ali to share a little about herself and how she ended up in her current position.

“I grew up on the East Coast in Philadelphia. Went to school at Rutgers in New Jersey where I was a meteorology major,” Ali began.

She always had an interest in the weather and was planning to be a broadcast meteorologist when she finished college. But her plans changed when Hurricane Sandy hit New Jersey during her Freshman year of college.

“You saw the destruction… you saw all the trees down, during the night transformers blowing up, huge lines at the gas station… so that really formed what I wanted to do with my life.”

After that Ali became more interested in flooding and the Oceans. She went on to study oceanography at Old Dominion University in Norfolk, VA where she earned a Master of Science.

“Norfolk, VA is home to the largest Navy base in the world,” Ali explained.  “So, as you can imagine, they were very interested in mitigating against sea level rise.”

Rising to New Challenges

After that, Ali moved to Washington D.C. as a Sea Grant Knauss fellow and was introduced to policy and worked on coastal resiliency issues.

“Then the pandemic hit, and I lost my job at the time,” Ali went on. “My friend was moving to Portland, and I always wanted to visit the west coast, so I packed up and came here.”

Finally, after a short stint at UC Santa Barbara, Ali was hired by Oregon State University in her current position—program manager for the Cascadia Coastline Peoples Hazard Research Hub, or Cascadia CoPes Hub.

“I have been there a year,” said Ali. “It has been a whirlwind of information… There are over 90 people associated with the project now.”

That is a lot to manage.

Ali Burgos posing for a picture on the promenade.

Collaboration

We hiked on, the sun warming us and the sand firm under our feet. Ali told me more about Cascadia CoPes Hub in fits and starts as we walked along taking in the scenery.

“In a nutshell, It’s a 5-year funded project from the National Science Foundation. We are trying to help coastal communities in the Pacific Northwest increase their coastal resiliency,” explained Ali.

Cascadia CoPes Hub is a newer collaborative (it started only about 6 months before Ali was hired) with multiple teams working on different aspects of coastal hazards research and outreach. Ali outlined the focus of each team.

Team 1 is geohazards. This team deals with research around earthquakes, tsunamis, and landslides.

Team 2 is coastal inundation. This team is looking at sea level rise, erosion, flooding, and overall storminess.

Team 3 is community adaptation. Team 3 wants to know what coastal communities are thinking—what do people value? What do they perceive as threats? And how do they get that information?

“This is where the social scientists live,” said Ali. 

Team 4 is the STEAM team. STEAM stands for science, technology, engineering, art, and math. And the goal of this team is to bring underrepresented students into STEAM through a fellowship program.

And finally, Team 5 is community engagement and co-production.

“Coproduction is kind of a buzzword in research right now,” Ali explained. “Coproduction is working outside your discipline or field to create new ideas, solutions, and knowledge.” It often involves working with communities, state agencies, as well as other academics.

“We keep growing… There were 60 people when I started, and now there are 90 plus.”

Fading from Gray to Green

As we hiked on the broad plain of sand, Ali pointed out just how low-lying the beach was.

“If you look at the beach here,” she remarked pointing about, “we are as flat as flat can be.” Not a good place to be if the water came up too high in a storm—not a lot of protection.

However, looking over toward the City of Seaside, a low wall wrapped along the promenade in front of all the buildings—wouldn’t that offer some protection?

“Over there we have some seawall,” Ali said, pointing to the structure. 

Ali referred to the wall as a form of grey infrastructure—a manmade structure built for, in this case, protection from flooding and storms. 

“I am not a fan, personally,” she went on. “It has its merits in certain situations, but seawalls can cause more erosion of the beach… And how tall do you make it?”

Seaside waterfront properties with seawall in front.

As if on cue, the open sand we were walking shifted—wide mounds of grassy sand dunes rose up in front of us.

“These are green infrastructure,” Ali explained. “This will help block wave energy during storms.”

Unlike seawalls, dunes collect sand, rather than letting it erode. As natural-based features, dunes can grow and change over time. “Plus, it can help with habitat,” Ali added.

“Natural and nature-based features are what people are going more towards,” said Ali.

Ali also mentioned cobble revetments as another example of grey-green infrastructure.  Essentially, a berm made of pebbles or cobbles mimics natural rocky beaches—water can move through the rocks, while sand can still build up.

“This is a great dune system,” Ali smiled as we headed through the dunes on what little beach was left. 

Low dunes along the northern stretch of the promenade.

On Shaky Ground

Soon the beach was all but gone and Ali and I decided to move to the pavement. We took some stone steps up and onto the Seaside promenade and continued our walk north.

As we walked, I asked Ali how she felt about the earthquake and tsunami hazards in the Pacific Northwest.

“It is definitely something I grapple with moving here,” Ali responded.

For those that haven’t heard, the Pacific Northwest is predicted to experience a high magnitude (possibly 9+) megathrust earthquake in the next 50 years. Current predictions estimate a 37% chance of a 7.1+ in the next 50 years according to oregon.gov. This will also result in huge tsunamis up and down the coast.

“What is most interesting about that is human perspectives—trying to understand how people see their vulnerability,” Ali continued. “It is easy to go day by day, especially if you don’t have past experience, to become very complacent.”

Sign at the end of the promenade marking the tsunami evacuation route.

Keeping Perspective

I asked Ali what she thought people should be doing considering the megathrust and tsunami risk in Oregon.

She suggested keeping things in perspective. Yes, there is a risk associated with visiting and living on the coast, but it is still very small.

“Even on my drive down this morning, I get anxiety about coming over here,” she confessed.

However, she also knows that the odds are in her favor.

“I am more likely to get injured in my drive,” she added.

So, what should people visiting or living on the coast focus on? Being prepared. That is what her research cooperative is trying to do—help people know how best to do this on a place-by-place basis.

“What is the most important thing to know to prepare?” I asked.

“I think the biggest thing is to know your evacuation route,” Ali suggested. “Many people don’t know which way to go, especially if you’re visiting.”

Whenever the Cascadia megathrust earthquake hits, there will be little time to move to high ground—perhaps as little as 10-20 minutes at best. So, look at the evacuation maps ahead of time and have a plan A and a plan B.

On cue, Ali and I reached the end of the promenade trail, where a tsunami evacuation map was prominently posted.

“Moving here, I learned a lot more about earthquakes and tsunamis than maybe I want to know,” Ali laughed nervously.

I hear that, Ali. 

Map of the tsunami evacuation route was posted at the end of the promenade.

Winter is Coming

Upon reaching the end of the trail, Ali and I about-faced for a return journey. This time we stuck to the paved walk that took us past the waterfront buildings—just a seawall in some spots for protection. Our conversation pivoted back to issues with high water. Ali was going to be speaking for the King Tides Community Science Initiative the following day about sea level rise, and with King Tides rolling in, it seemed important that we return to coastal inundation. Plus, I had a lot of questions.

On the top of my mind was winter—why were king tides so notable in the winter? I asked Ali.

“They are worse in the winter,” she responded, “because of the Earth’s orbit around the sun. We are closer to the sun in the winter so the gravitational pull is stronger… winter king tides are going to be stronger.”

One of the biggest Earth Science misconceptions is that the Earth is farther from the sun in the Northern Hemisphere winter, resulting in a change in seasons, but the opposite is true. Fun fact, seasonal shifts have more to do with the tilt of the Earth in relation to the sun. (You have just been scienced!)

Additives

Then of course there are the potential additive effects of storms which are more common on the Oregon coast in winter. I asked Ali to explain how storm surge and waves play a role in water levels.

“Storm surge is basically when you have a storm coming up the coast. You have low atmospheric pressure… with a lot more wind. The winds and pressure are forcing the water up—that is basically your storm surge. This can be coupled with high tides, which could make flooding worse.”

Ali explained how the wind is a result of pressure differences along the Earth, which are greater in the winter. And high winds equal bigger waves, which have harmful effects.

“Winter storms come through and produce a lot more wave energy,” Ali explained. “Those big waves can move sand around, cause erosion, and bring in a lot of debris.”

Both storm surges and big waves happen all the time, but with high tides, the consequences are magnified.

Rise Up

So, what about sea level rise, overall? What can we expect there?

There are two major contributors to sea level rise, according to Ali: 1) melting glaciers from Greenland and Antarctica, and 2) warming oceans.

How melting glaciers contribute to sea level rise is straightforward: glaciers add water from the land into the ocean, literally filling up the global bathtub, as it were.

Warming oceans affect sea level in a different way—causing the same amount of water to take up more space. As the water warms, the water molecules move apart in their higher energy state, taking up more space—something called thermal expansion. 

Variability

Of course, there is some variability.

“Thermal expansion and ice melt aren’t uniform,” explained Ali.

Plus, there are other factors having an effect including changes in currents due to climate change and differences in vertical land movement.

There are sea level rise hot spots, as well as places that aren’t seeing any sea level rise at all.

Luckily, sea level rise has been slower along the Oregon coast overall—mostly because the land is rising too, counteracting sea level rise in some locations.

“Global mean sea level rise is 3.4 mm,” said Ali. “Oregon is not anywhere near that.”

Another El Niño

Then there is natural variability related to whether we are in a La Niña or El Niño year.

“ We have been in a La Niña for the past three years,” explained Ali.

La Niña brings colder weather and more precipitation to the Pacific Northwest.

“Which is great for skiing,” she chimed.

In an El Niño year, the oceans will warm—which could lead to greater thermal expansion and other issues associated with a warmer climate.

“And with climate change,” Ali added, “they may become more frequent and more severe.

“The biggest thing with sea level rise is your basic water gets higher—everything is happening on a higher base,” Ali explained.

In other words, a higher sea level means a higher storm surge and high wave energy eroding places it never reached before. King tides would be higher than they are now, and the next El Niño year, more severe. 

Act Now

“What should we do?” I asked Ali.

“Our oceans are rising, that is fact,” Ali responded. “How much and when, is the biggest thing to think about, and what do emergency managers need to think about.”

More specifically, Ali recommended creating more natural and nature-based features on the coast as the first line of defense against inundation.

Another option—is managed retreat. Managed retreat is a planned process of moving buildings and people further inland to avoid hazards and risks.

“Managed retreat isn’t popular, but something to think about,” said Ali.

Ali was quick to add that, managed retreat isn’t something that she is in a rush to see happen in Oregon. Oregon isn’t facing a sea level rise crisis currently, so it probably isn’t as important a strategy right now. However, in the broad scheme of things, Ali was clear that managed retreat is important to adapt to sea level rise. 

Predicting the Future

We were nearing our starting point on the promenade when we passed by a decorated tree or bush opposite the seawall. I snapped a picture. It seemed important for some reason. An emblem of the community perhaps?

Considering the community, what is the future of sea level rise?

“Sea level rise is exponential right now,” Ali told me as we walked. “Not on a linear increase. The rate is getting faster.”

“Why is that?” I asked.

“Warming and melt is on a lag, “ Ali explained. “Even if we stopped emissions right now, the oceans will continue to rise.”

And continue to rise, in theory, indefinitely.

“It is hard sometimes,” Ali paused. “People say ‘you are just doom and gloom’… There is a fine balance to walk—understanding the risks but knowing there is something we can do.”

Holiday “tree” along the promenade.

 Incoming Storm

Ali and I were still discussing sea level rise when we got to the point where we could see the waves and an access point to the beach. 

“The water is straight up to the edge,” Ali proclaimed referring to our coastal view. “High tide today is about 8-9 feet. It is normally 2-4 feet.”

We headed down to check out the waves from a better vantage point.

As we walked out toward the pounding waves, Ali told me more about ocean waves and how they are generated.

“The wave energy is coming from the wind,” she began. The longer the fetch (the length of water that the wind can blow without being blocked) the more energy can be imparted into the ocean allowing waves to grow larger.

She went on to explain how the low-pressure system that generates the storm also has a small effect by pushing water up due to the inverted barometer effect.

“If you have low pressure the water is going up. High pressure it gets pushed down,” Ali described. 

All that said, it was clear to Ali that a storm system was on its way.  Waves were rushing up fast, breaking quickly, and curving ferociously—all signs of an incoming storm.

“They [the waves] are definitely stronger,” she remarked as we stopped and stared. “And it’s happening pretty far offshore… and getting those nice curves to them.”

I looked out toward the ocean to try and see what Ali was seeing. I hadn’t considered this idea before—that I could look at the ocean and predict the future.

Staring out at the rhythmic movement of the incoming waves—it all started falling into place.

Reflections

Our oceans are sending us warning signals. They warn us of storm systems coming through hours to days in advance. But more than that, they warn us of impending changes to our planet that we can’t afford to ignore.

Visiting the coast during king tides can be a lot of fun—people flock to the coast to see the massive waves and enjoy the pounding surf—but they are also a reminder that our planet is changing. 

Our oceans are warming quickly, and the global sea level is rising, resulting in a multitude of changes to Earth and human systems.

The signs are there. We just need to learn how to see them.

Alessandra (Ali) Burgos a project manager for Cascadia Coastlines and Peoples Hazards Research Hub with Oregon State University. Ali earned a Bachelor of Science in Meteorology at Rutgers University and a Master of Science in oceanography at Old Dominion University.

Hike with a Meteorologist

View from upper Rodney Falls looking down.

The sky was crying out large splattering raindrops quicker than my windshield wipers could sweep them away. Traffic was usual for a Sunday morning in Portland, Oregon, as I headed north on I-205, and eventually into Washington state. My destination: Hamilton Mountain Trailhead. My purpose: to meet up with meteorologist and fair weather hiker, Steve Pierce, for an afternoon hike and interview. 

But the rain was hammering and I was beginning to wonder if this thing would happen. Steve had told me straight-out-of-the-gate that he didn’t hike in the rain, so he probably wouldn’t be up for a downpour. 

What is up with the Weather?

Weather: atmospheric conditions present at any given time, on any given point on Earth. Such a simple definition for such a complex, life-altering phenomenon. The weather can turn a good day into a bad one, build up our snowpack, exacerbate forest fires, leave us exposed, fearful even. And in my case, possibly defer a hike?

The weather was doing its thing. So I drove and crossed my fingers (figuratively), tracing the path of the Columbia River to my right as I headed east on Highway 14. By the time, I reached the trailhead, conditions weren’t looking much better. By the time Steve pulled up in his little red convertible, we were still in the thick of it.

Windows rolled down and raindrops falling all around, I met Steve Pierce for the first time, sitting side by side in our vehicles. After some quick introductions, he pulled out his phone to check the weather radar. “Another 15 minutes or so and the rain would pass,” Steve told me with confidence. 

A Career

The hike was on. We just needed to wait out the rain for a bit. So Steve slid into my car and told me how he got started in the world of weather.

Beginnings

Inspired by events like the 1980 Mount Saint Helens eruptions, from a young age Steve was interested in weather. “I was fascinated with which way the ash clouds were going,” said Steve.  When ash fell in the Vancouver-Portland, Steve was only seven but he remembers the experience vividly.  In particular, he recalled spending time with his brother sliding around on their bikes on a slurry of ash and water that felt akin to snowfall. Coupled with a couple of major snowfall events earlier that same year, the appeal of meteorology hung heavy in Steve’s young mind, like (dare I say) rain in a cloud-ready to fall. 

Self Taught

Throughout his youth, Steve studied the weather on his own. He read every book he could get his hands on, including every meteorology book at his local library. Later, when the internet was a thing his studies continued. 

Early on he also tried his hand at forecasting. In 5th grade, he started writing a weekly weather forecast for his elementary school’s parent bulletin. At home, Steve would broadcast the weather from the family fireplace hearth through his Mr. Microphone. He also had a weather station and was a devoted weather spotter for Channel 8. By 9th grade, he found himself on the cover of the regional paper (The Columbian) in an article titled: “Teens Career Forecast is Clear.”

You’re Hired

Fast forward to 2014, after attending Mt. Hood Community College (1994) and Washington State University, Vancouver (2001), a family, a prior communications career, and“fever” for investing in real estate, Steve finds himself at a crossroad in his life. At this point, Steve is an active member and President of the Oregon Chapter of the American Meteorological Society (AMS), but otherwise had made his career outside of meteorology, when he gets “the call.” It was local news anchor, Jeff Gianola, who remembered him from 20 years prior, when Steve was a college intern, with a job opportunity: Meteorologist for KOIN 6 News. Steve is instructed to: “get on a suit and come to the station” if he is interested in this rare opportunity. Adorned in basically the only formal suit Steve owned at the time, he goes into the station for a mock-up weather forecast. He is hired on the spot!

Time to Hit the Trail

This brings us to today.  Steve and I had been talking for several minutes in the car at this point so that the windows were fogged up and the air a bit warm and humid. The rain, on the other hand, had finally stopped. I suggested that we hit the trail. 

Steve Pierce at the Trailhead

The Hike

  • Trailhead: Hamilton Mountain Trailhead
  • Distance: approximately 2.5 miles round trip to Rodney Falls
  • Elevation Gain: approx. 450 feet elevation gain
  • Details: The trail to Rodney Falls is an easy out and back hike. Those that want more of an adventure may continue to the top of Hamilton Mountain for a total of 7+ miles and 2100+ feet elevation gain . There is ample parking at the trailhead and restroom facilities available. Parking requires a WA Discover Pass.

Basic Science 

Steve and I started our hike with a couple of photos before making our way up the forested trail. The sun was coming out and the only water falling around us was from the surrounding vegetation.

“See I promised it was going to be good,” Steve smiled. 

As we moved at a quick pace, I asked Steve to tell me about what it takes to understand the weather. What does it take to forecast the weather? He said two things: 1) basic science and 2) interpreting computer models. 

“Anyone can be a weather enthusiast,” replied Steve, “but sort of where-the-rubber-meets-the-road is really understanding meteorology on a scientific level. How are weather patterns created? How do they evolve?”

He went on with an example. “We live in a part of the country where the Columbia River Gorge is huge in determining our weather. Without the Gorge, we would rarely get snow in Portland.” He explained that the Cascade mountains create a barrier that separates the cold, dry continental air mass that sits over the continent during the winter. The Gorge is a gap in that barrier. “The gap is how we tap into that cold air.”

And this is where we get into some of the basic science of meteorology. Cold air is dense and tends to sink, and warm air rises and expands. Air also moves from low to high pressure.

So, if we look at the science, it makes sense that in the winter, the cold air from the east would be more than happy to rush through the Columbia River Gorge following the pressure gradient, on its way to the relatively warmer ocean. Then, if there is some moisture on top of that, bring on the snow! 

Computer Models

In addition to knowing the basic science, “interpreting computer weather models” is essential to meteorology, especially in modern times. 

Computer weather models take observations from weather stations and weather satellites and assimilate them into a 3-D grid. They then use mathematical equations that describe the physics of atmospheric variables, like pressure, temperature, wind, and moisture, to make predictions about future atmospheric conditions. Thus, weather models depend on both the equations used and the observation. The better both of these play together the more accurate the forecast. 

Steve shared that the models he prefers are a set found at the University of Washington, developed by “long-standing atmospheric science professor, Dr. Cliff Mass.” NOAA also has some high-resolution models too. 

Computer models have truly revolutionized weather forecasting, making accurate forecasting possible. This is the “leading-edge technology” we are talking about. Available to all, these models make forecasting the weather a breeze (pun intended) compared to the past. The Labor Day winds and forest fires, for example, were forecasted to the hour by weather models.  

Again, most of these models are available for those who are interested. 

Why Weather?

And who isn’t interested? 

The weather has always been kind of a big deal—affecting our past, present, and future. 

As Steve puts it, “Weather affects everybody. It affects your everyday life, your job if you work outside—agriculture, for instance.” The weather today can also affect the future. 

For example, the amount of winter snow in the Pacific Northwest, predicts future water supply in the region. All that snow that dumped down in the valley and mountains a few weeks ago wasn’t just weather for now, but water for later. We even saw remnants of the snowfall during our hike along the trail. 

“I just saw the latest snowpack for Mt. Hood,” said Steve, “and we are at 100-110% of normal.” And that is good news for the upcoming summer water needs across the Pacific Northwest.

Snow on the trail!

A Tale of Two Clouds

The forested trail continued into a short clearing where I could feel the sun warming my skin. In his cavalier way, Steve noted this change in weather. He had promised it would be nice.

To the right, there was a bit of a view out toward the river and a basalt cliffside, but my attention was drawn to the clouds overhead. I asked Steve, “What kind of clouds are these?”

“These are cumulous,” replied Steve. 

Clouds are a personal favorite of mine. And growing up in Oregon, there never seems to be a shortage of clouds to look up at. So of course, I needed to know more, so I asked Steve to elaborate. 

As he explained it, there are many types of clouds, but two of them are the most interesting to him: cumulus and stratus.

Cumulus

Cumulus clouds, like much of what we saw during our hike, are convective. What does that mean? It means that the droplets of moisture that make up the cloud are heated up by the surface of the Earth and rise up. Just like a pot of boiling water, cumulus clouds “puff-up” as they rise, like bubbles breaking the surface. Cumulus clouds are also a sign of an unstable atmosphere and that severe weather may be on its way.

Stratus

Stratus clouds on the other hand are low to the ground. Unlike cumulus clouds, stratus clouds are stable and flood in from coastal areas in thick layers of moisture.

According to Steve, “Stratus are unique to the west coast.” During the summers, the air above the ocean is colder and denser than inland. This colder air can be held at bay during the day, but by 6 p.m., as Steve puts it, “mother nature’s air conditioning kicks in,” and the cooler coastal air drifts inland through gaps in the coast range, including the Columbia River Gorge. Oftentimes, this cool onshore flow will also bring in stratus clouds, filling-in the valley overnight. 

Viewpoint with some “dissipating” cumulus clouds

Clashing Air

While cumulus clouds continued to drift east through the Gorge, Steve and I continued our hike in the same direction, leaving the cloudy peek-a-boo view behind.  

Moving swiftly up the trail now, my mind was racing, as I attempted to assimilate all that was being said. One word stuck in my mind: “unstable.”  Steve had thrown this word around a bit. If today was “a bit unstable,” as Steve suggested, what does that mean? So, of course, I asked. 

“An unstable air mass, simply put, is very buoyant air,” Steve replied. “Unstable air is usually what follows a cold front. And a front is the clash of two air masses, warm air ahead and cold air behind.” The clash between the cold and warm air builds up clouds as the colder, denser air mass replaces the warmer, less dense air mass, resulting in cooling and condensing of water droplets that form clouds and can produce rain.

A Big Difference

Steve further explained that the bigger the difference in temperature between the air masses, the more unstable the air mass can become. And the greater the instability, the bigger the potential for convective storms.

In the Pacific Northwest, the biggest storms tend to occur in the spring as there is more heating of the Earth by the Sun, creating more frequent and larger temperature differences between air masses and in between the different layers of the lower atmosphere, say below 25,000ft.

Extreme Weather

However, despite the Pacific Northwest’s reputation for weather in the form of rain, we do not have the extreme weather that you might see, in say, the midwest. 

In the midwest, supercell thunderstorms develop and spin up tornadoes because of the clash between cold continental air from Canada and warm air from the Gulf of Mexico. In the Pacific Northwest, this sort of instability just doesn’t happen often. The differences in temperatures over the Pacific Ocean land are just not that significant. As Steve put it: “We just have relatively cold” air.

Cold to the Core

Instead, the Pacific Northwest’s version of a twister is a much calmer cousin—the cold-core funnel cloud. A cold-core funnel (while also sounding like a new exercise routine) is the Pacific Northwest version of a tornado. Simply put, it is a vertical “rotating” column of air in the atmosphere that is especially cold, unstable, and almost always trails just behind the recent passage of a cold front.

“After a front has passed, we typically have westerly flow at the upper level of the atmosphere, and a southerly or southwesterly flow up the Willamette Valley”, Steve explained. “Just enough wind sheer between the two, along with geographic enhancements in the valley, and you can spin up a horizontal column of unstable air and then turn that column vertical due to the wind sheer present.” Hence, a tornado.

If these cold-core funnel clouds touch down, though rare, they can cause EF-0 or EF-1 tornado damage. 

In fact, according to Steve, the deadliest tornado west of the Rockies hit Vancouver, WA on April 5, 1972. Rated as an EF-3 (F-3 back then) tornado, winds were 165-210 miles per hour. Six people died that day in Vancouver when a supermarket and bowling alley roof collapsed. The roof and walls of near-by Peter S. Ogden Elementary School were also damaged.

Large Bodies of Water 

However, deadly storms are anomalies in the Pacific Northwest. “We don’t really have that kind of volatile weather,” explained Steve, “because we have the Ocean.” The Pacific Ocean, as is the case with any large body of water, is slow to heat up and slow to cool down, making it an excellent moderator of climate. 

In the summer, when the inland starts to heat up, the Ocean lags behind. In the winter, temperatures drop inland, but the Ocean retains its heat. The result is cooler summers on the coast and warmer winters.

The moderating effect keeps Portland and other Willamette Valley temperatures from reaching extremes as well. Hiking in the Gorge, even in early March, is pleasant and cool, but not too cold (at least relatively), all thanks to the Ocean to the west. 

Weather Patterns

One of the first things Steve talked about when I asked him about his interest in meteorology was the importance of weather patterns. 

Here is what he said:

“What I am most passionate about with meteorology is I know things happen in cycles. In other words, when we saw the big snow event coming just a few weeks ago, I thought back to previous events where I knew this happened in the past… I remembered I have seen this pattern before. Weather is a set of different patterns that come and go.”

In Oregon, typical patterns of weather result in a climate that is warm and dry in the summer and cool and wet in the winter, and overall pretty moderate. But, on the other hand, we can also predict deviations from the norm, like the winter storm Steve explained earlier. 

Much too Hot

Another example of these patterns of predictable deviations occurs in the summer. 

Typically during the summer in Oregon, there is a ridge of high pressure over the ocean that blocks storms between June and October, while prevailing winds from the northwest, carry cooler ocean air onshore as a high-pressure system spins clockwise in the northern hemisphere.  This is the norm.   

However, there are also usually a few days of 90+ degree days, where things don’t cool down.   In Oregon, you can expect a couple of brushes with high-temperature days in the summer—it’s a pattern. This occurs when a low-pressure system from the Southwestern United States creates a thermal heat trough that moves into western Oregon. This turns the airflow counterclockwise, directing the winds offshore toward the coast. Not only that, but the downslope flow of air of the Cascade mountains results in “compressional heating,” a thermodynamic process that heats up the Willamette Valley of Oregon even more. 

A Numbers Guy 

Now one thing that became pretty obvious early on is that Steve is a numbers guy. He is self-professed “good with numbers” and bad with names. I am not great at either so I was impressed how easily he rattled off dates when I can barely remember my own kids’ birthdays.  

“Hottest temperature in Portland: 107o F on August 10th, 1981,” Steve rattled off as we marched along.  “Coldest temperature in Portland: -3o F on February 2nd  1950.”

After tip-toeing our way through a mud patch, he went on:

“Average temperature in Portland is about 53o F… about the same temperature as the Pacific Ocean… It balances out.”

Superlatives

Steve continued with the superlatives:

  • Wettest months: November & December (a near “tie” at 5.60” and 5.40” respectively).
  • Most active weather (thunderstorms): March through May
  • Foggiest month: October
  • Biggest change in temperatures: Also October. “With an average range of high’s from 71o F on the 1st to 58 o F on the last day of the month.”
  • Best Month: October (in Steve’s opinion, due to the change of season and falling of leaves)

Chasing Waterfalls

As Steve and I waxed poetic about the beauty of fall foliage in the Pacific Northwest, the rushing sound of water filled our senses. We were nearing the base of the middle of Rodney Falls located on Hardey Creek. Here, we decided to stop the interview for a bit to check out this fun natural feature.  

Steve and I first took an upper trail to the left to get a close view of one of the tiers of the multi-tiered waterfall, before heading down to the base of the fall where you cross over Hardey Creek to continue the hike. With so much snow and rainfall recently, nature’s tap was on full blast and the falls were spectacular. 

Rodney Falls

A Cliffside View

Just beyond the falls, Steve and I continued our hike a few hundred feet up to a viewpoint looking out at the Columbia River Gorge. From here you could see the north-facing wall of the canyon rising up on the Oregon side of the Gorge, still covered in snow. 

Looking out at the basalt rock cliffs, Steve and I shifted our discussion toward the landscape. (Literally, as we faced the canyon wall.)

“Geographic features have an effect on weather patterns,” Steve said. The Gorge plays a part in shaping weather patterns in the valley. The Pacific Ocean moderates temperatures all along the western margin of the country and beyond. 

View of the Columbia River Gorge just above Rodney Falls on the trail

Rain Shadow

There are many geographic features that influence the weather in any location, but one that is particularly important to the Pacific Northwest is our mountain ranges. The Coast Range and the Cascade Range both run north-to-south in the region, creating barriers for winds and weather. 

Mountain ranges, like those in Oregon, create what is called a rain shadow—a dry landmass on the opposite side of the mountains from which the air is flowing. As cool, moisture-rich air from the coast travels up each mountain range’s western flanks (also known as the windward side), the air cools and moisture condenses forming clouds and precipitation. Once the air makes it to the eastside (also known as the leeward side), the air has been wrung out like a sponge. As the air descends further it also heats up and evaporation increases. 

In Oregon, this means that it gets drier as you head east across the state. According to Steve, the coast averages 60 inches of precipitation, Portland 37, and Bend less than 10. 

This also means that in the east you experience a very different ecology than in the west. Instead of the shaded, wet Douglas-fir forest, we were hiking through, hiking the east would take you through open, dry shrub-steppe habitat, or perhaps a Ponderosa Pine forest. Hiking in the east means applying a lot more sunscreen and packing more water. 

Douglas-fir trees line the muddy trail.

Sunrise & Sunset

After sufficient time at the viewpoint, Steve and I decided it was time to turn around and head back. And as the sun was setting on our time together, I couldn’t help but ask Steve about literal sunsets—can we use the weather to predict the best sunrises and sunsets?

Yes you can! 

“The first thing I would do is look at satellite imagery,” said Steve, “…nothing coming off the coast is a good sign.” If there is a ridge of high pressure over us that shuts down the onshore flow that equals a good sunrise or sunset. 

Steve also recommended winter, as the best time to see sunsets. “The atmosphere is more mixed up,” he explained, “so you get really clear air.”

He also warned that sunrises can be more tricky though because of the morning stratus clouds that move off the coast and through the valley at night. These clouds can put a damper on a good sunrise. Of course, when in doubt you can always head east. The clouds can’t make it inland that far. 

The Road Home

After Steve and I finished our hike, I climbed back into my car and began the long drive home west through “the Gorge” and south into “the Valley.” 

On my way home the pleasant weather turned from partly cloudy to stormy in what felt like an instant. Hail fell from the cumulus clouds overhead and I am pretty sure I saw a flash of lightning off in the distance. Steve was also stuck in Washougal, WA. by a torrential downpour, thunder, and lightning.

The stormy weather was short-lived, however; and as I pulled into my neighborhood the sun was setting, turning the clouds a soft shade of pink. Seeing the painted sky brought me a sense of calm following the chaos of the weather-filled day. I thought, “How very appropriate; this is what it is like to hike with a meteorologist.” 

Steve Pierce is a part-time meteorologist at KOIN 6 News based in Portland, Oregon. He grew up in Vancouver, WA where he first developed a passion for weather. Steve studied Television Production at Mount Hood Community College and Business and Communications from Washington State University, Vancouver. He is also the President of the Oregon Chapter of the American Meteorological Society since 2012.