Early September Bearcam Questions and Answers

This blog has been relatively dark over the last year, not because I hadn’t intended to write for it but because I frequently had other writing duties to fulfill. Afterward completing one task, it was often easier to space out at the end of the day than concentrate on writing something that approaches partial intelligence.

I want to share a little of what I have been writing though. Each Tuesday, I cohost a question and answer session in the comments on explore.org’s Brooks Live Chat channel. It’s an AMA about anything related to Katmai National Park’s bears and salmon. Many people submit your questions in advance, which allows me to answer them with greater detail than a question asked on the spot. Below are my answers to those questions during the Q&As for early September.

Be sure to join the Q&A every Tuesday from 5 -7 p.m. Eastern in the Brooks Live Chat channel, and if you prefer to chat in sentences limited to 200 characters, then join the bearcam conversation on explore.org’s Brooks Falls YouTube feed.

September 1, 2020

I’d like to talk about the “Beaver Pond,” which Kathryn asked about via the Ask Your Bearcam Question form. “I’ve often looked at photos of the [Beaver Pond] and wonder if any salmon can make it to the pond and if any of you have seen bears fishing or hunting around the pond?”

The “Beaver Pond” is located about fourth-tenths of a mile south of the outlet of Brooks River. A road provides an avenue to get near there although there is no developed trail to the pond’s edge. Bears use the area but mostly as part of their efforts to get to and from Brooks River because the pond is inaccessible to salmon.

The Beaver Pond in relation to Brooks River
A beaver at the Beaver Pond

Beavers maintain a lodge on the pond’s north side and a grass-covered dike (an old beaver dam) lines much of that area. But, the Beaver Pond isn’t a true beaver pond in the sense that its formation was the direct result of beavers. It was once part of Naknek Lake and has since been cut off by the sediments deposited by wind driven waves.

The beaver pond was once a cove on the edge of Naknek Lake. Strong easterly winds create waves that erode the gravel shoreline to the southeast of Brooks River. The waves carry gravel and sand northwest toward Brooks River. Over time, a horsetail shaped beach began to encircle the cove.  This image below is from an unpublished geologic report about the Brooks River area. Note the concentric ridges along the lakeshore near the beaver pond. These are the beach ridges that cut off the beaver pond from Naknek Lake.

This process is similar to what we see at the river mouth, especially in the “spit” area that partly encloses a lagoon-like area rangers call the boat cove. The boat cove may be destined to become a small pond or marsh like the wetlands between the river mouth and the beaver pond today, although the mouth of Brooks River is more exposed to direct blows from wind-driven waves than the beaver pond area. Strong storms can quickly rework and reshape the gravel at the river mouth.

In the above image, the parallel lines farther inland are old beaches as well, although they weren’t formed by longshore currents. Instead, they mark the former levels of Naknek Lake and Lake Brooks. Naknek Lake has been slowly lowering in elevation as Naknek River cuts through the glacial sediments that dam the lake.

Although we don’t know exactly what the Brooks River mouth area will look like in the future, we definitely know it will not look the same.

Jen wrote in wondering about the line-up of salmon we sometimes see below the river watch cam and asks, “Has that behavior been noted before?” And, “What criteria initiate egg-laying?”

This is the formation that Jen refers to.

Parallel lines of sockeye salmon in Brooks River. The fish are facing upstream and in this image the current flows from right to left.

Sockeye salmon line up in fairly parallel rows frequently in late summer in the lower Brooks River. Until this year, however, with more salmon using the channel below the river watch cam, we haven’t been able to see this on the cams very well. Although this is not a new phenomenon at the river, I haven’t been able to find an explanation for it. We know the salmon are staging (waiting for the right time to spawn) but I don’t know if lining up in rows gives them any sort of advantage. It may be the most efficient way to sort themselves or there could be some social cue among the fish that prompts the formation. It’s a beautiful feature of the lower river in late summer.

Regarding Jen’s second question, a female salmon lays her eggs in nests she constructs by fanning the gravel with her tail. This action winnows away fine sediments that might hinder water flow (and hence dissolved oxygen) around her eggs. She’s looking for gravel of the right size and in areas of the river with consistent water flow. Males will fan the gravel occasionally too but they play no role in nest construction. Once the female determines her nest is suitable and she’s accompanied by a suitable male, she’ll release her eggs directly into the nest while the male releases his milt. In this way, it is the female who determines when to lay eggs.

LoveTheBears writes, “I understand that there is an area designated for cleaning any caught and kept fish.  What happens with the discarded fish parts?”

There used to be a public fish-cleaning building at Brooks Camp. The first iteration wasn’t much more than screened-in shelter with a bucket on the floor where people disposed fish entrails. It was later replaced by a more substantial log cabin style building where people could clean their fish. Today though, there is no public fish cleaning facilities at Brooks Camp and the public is prohibited from cleaning fish within 1.5 miles of Brooks Falls. People can keep one fish per person per day downstream of the bridge, but they must take it immediately to the Fish Freezing Building (the old fish cleaning building) and place it in a freezer. It must remain there until you depart Brooks Camp.

Although no bears at Brooks River are currently conditioned to seek human food, it hasn’t always been this way. In the 1960s and 1970s, many bears learned to associate people with food and sought opportunities to get at human foods at Brooks Camp. The fish cleaning buildings were part of the issue along with open dumps, outdoor burn barrels for garbage, and overall lack of awareness and regulations about proper food storage in bear country. As part of the effort to reduce the risk of bears becoming food conditioned, the NPS got rid of the public fish cleaning facility.

Bears easily learn and remember any trick that allows them to find food. Therefore, we must remain constantly vigilant to ensure that bears don’t learn to associate us with fish. The NPS and the State of Alaska implemented somewhat strict fishing regulations in the 1990s, which has greatly reduced the number of incidents when bears have learned to associate people with fish. Eliminating public fish cleaning facilities and prohibiting fish cleaning within 1.5 miles of Brooks Falls inconveniences some people but it is a big step toward protecting bears.

September 8

Angela writes, “We were talking about hibernation in the chat thread and wondered if it is necessary for bears to hibernate. We understand that bears at Katmai hibernate, but were wondering if bears in captivity also hibernate or if because there is a regular food source, the need to hibernate isn’t triggered?”

Hibernation exists along a spectrum rather than being an either/or behavior. Some mammals such as arctic ground squirrels are obligate hibernators, meaning they hibernate regardless of ambient temperatures or access to food. Bears experience a type of facultative hibernation. Given the right circumstances, bears needn’t hibernate to survive winter.

Each year, at least some black bears in mild climates (Sierra Nevada foothills, coastal plain of the southeast U.S., and Big Bend National Park to name a few) remain active all year. These are generally adult males. Similarly, a few adult male brown bears are active on Kodiak all year. Mild temperatures and at least some food allow these bears to remain out and about.

In North America, only pregnant female bears must enter a den and it isn’t because they must hibernate. Bear cubs are born so small and physically immature that they need many weeks of additional development before they are mobile enough to travel with mom. This is even true of polar bears who utilize the winter season to hunt seals on sea ice. Instead of heading out on to sea ice in early winter, pregnant female polar bears, just like all other pregnant North American bears, head to dens to give birth.

Although a handful of bears remain active all year, especially in more southerly populations compared to Katmai, hibernation is a bear’s best energy conservation strategy. It makes sense for nearly all bears to hibernate during winter when food is either very limited or non-existent. For those bears who stay active (other than polar bears), their metabolism and activity rates are much lower than summer. Winter activity, therefore, doesn’t mean that bears are as active as they would be in summer. So even captive bears may ignore food and water provided to them, relying more on their hibernative physiology to survive.

Erin asks, “747 is a huge bear. Is he the biggest bear seen at Brooks River? Have there been bigger bears in the past?”

As I’ve said and written many times, 747 is a giant of a bear. He is the most massive bear I’ve ever seen and we should not take his presence for granted. If 747 were to disappear from the river, it may be a long while before we see another as big as he. Last year, 747’s was estimated to weigh more than 1,400 pounds.

747 from Fat Bear Week 2019

Each year, there are comparably sized bears in Katmai and at Brooks River. I’ll start by listing three of the currently seen bears who approach 747’s size class and then highlight two who might have approached it in the past. Only the largest adult males are comparable.

Right now 32 Chunk, 151 Walker, and 856 are close to 747’s size (at least within 300 pounds or so). They certainly rival him when measured by height and length. Each of these bears seem smaller to me than 747, but looks can be deceiving. Size is also an important determinate of dominance in the bear world. It is not absolute though. While 747 is more dominant than Chunk and Walker, 747 consistently yields to 856.

32 Chunk from Fat Bear Week 2019
151 Walker from Fat Bear Week 2019
856 from Fat Bear Week 2018

In the past, Brooks River has hosted some very big bears. While I never had the opportunity to see Diver in person, he was reportedly extremely fat and large in his heyday during the 1980s and 1990s. Look at this photo as an example.

In 2007, the most dominant bear I saw at the river was 24 BB. He was very tall and long–so a massively framed bear. He didn’t use Brooks River in late summer though so we never got to see BB at his peak size for the year. BB behaved much like 856. He asserted his dominance frequently and spent less time fishing than 747 does today, so he might not have been as heavy as 747 but the potential was there.

BB in July 2007

Marlene writes, “856 is getting older. I am wondering if he will know when he no longer can hold the top spot or do you think there will have to be a confrontation?”

856 has been the river’s most consistently dominant bear since 2011. Like all bears, 856 is great at weighing risk versus reward. For him, the overall risk of confronting other bears is low and provides great reward in the form of access to food, fishing spots, and mating opportunities, because other bears recognize his dominance. 856 will use that to his advantage as long as he can.

His high level of dominance is tied to his health and fitness. He’s a large bodied bear so will remain relatively dominant no matter what but he needs to maintain his good health and fitness in case another bear challenges him or is unwilling to yield. 856 might fall from the top of the hierarchy if he is defeated in a fight by another comparably sized bear.

His reign as the river’s most dominant bear could end in another way though. He might not feel up to the challenge.

In July 2017, 856 was an infrequent visitor in July and when he did show up, he yielded easily to 32 Chunk, perhaps because he suffered from a leg injury that hindered his ability to compete with other comparably sized males. At the time, already after many years of dominance, I thought this was the end of 856’s reign at the top. I was wrong. 856 returned to the return to the river in September 2017 looking as healthy as ever and acting as dominant as ever. He hasn’t taken a step back since.

The chances of a repeat of July 2017 could be in 856’s future just as much as his defeat in an intense fight at the paws of another bears. If 856 continues to return to the river as he ages into his early and mid 20s, I think we’ll see at least one of those scenarios play out.

Mount Katmai Caldera

We found ourselves hanging over the brink of an abyss of such immensity that, as the event proved, we were powerless even to guess its size. Down, down, down, we looked until the cliff shelved off and we could follow it no further.

–Robert Griggs in The Valley of Ten Thousand Smokes describing the moment he first peered into Mount Katmai’s caldera

Standing on the rim of the Mount Katmai caldera, staring at the gaping hole where a mountain once stood, elicits a profound awe. At the caldera and across the Valley of Ten Thousand Smokes, the Earth’s power and ability to foment change is laid bare.

About a year ago, I disappeared into one of the most unique landscapes on Earth, the Valley of Ten Thousand Smokes in Katmai National Park, a trip I partly chronicled in a blog post for explore.org. I hadn’t specifically planned on ascending to the caldera rim on that trip, knowing that the weather along the crest of the Aleutian Range is fickle at best and an inviting window of opportunity may never materialize. When I woke at daybreak on June 10, 2019 to see a cloudless sky though, I left my base camp eager to reach one of Katmai National Park’s most spectacular features.

I slept the previous night at Novarupta, the lava dome that marks the eruptive center of the 1912 Novarupta-Katmai eruption, the largest eruption of the twentieth century and one of the five largest volcanic eruptions in recorded history. The lava dome represents the eruption’s last gasp, forming anywhere from days to months after the 60 hour eruption waned on June 9, 1912.

view of pumice-covered flats and snow fields dark-colored lava dome at center

Novarupta lava dome

I began walking not long after the first light of dawn cast a pink alpenglow on the surrounding volcanoes. The rivulets of snowmelt where I gathered drinking water the prior evening had run dry as overnight temperatures dropped below freezing. Thankful for the firm footing, however, I traveled quickly across frozen snowfields to the base of the Knife Creek Glaciers, a badlands of pumice-covered ice attached to the north faces on Trident and Katmai volcanoes.

view of snowfields and mountain peaks

Early morning light on Trident Volcano

Not one, but many meltwater streams pour from the snout of these glaciers, and the permanent channels have eroded deeply into the pyroclastic deposits that form the Valley of Ten Thousand Smokes proper. Finding places to hop over or ford these streams is straightforward, although tedious work as you climb in and out of their past and present floodplains. They can be crossed most safely within a few hundred yards or less of the base of the ice. Farther downstream, they create impassible gorges, akin to southern Utah’s famed slot canyons only filled with a torrent of glacially cold water.

view of pumice flat and small stream with ash and pumice covered glaciers in background

Lower sections of the Knife Creek Glaciers are a badlands of ice covered with as much as six feet of ash and pumice.

Compared to the scale of geologic time, Katmai’s volcanoes forced their way to the surface relatively recently. Over the last several hundred thousand years, upwelling magma buckled and fractured its way through thousands of feet of Jurassic-aged rocks, although these sedimentary layers have deformed little since they were deposited. The rock of “Whiskey Cleaver” a wedge of 150 million year-old marine sediments buttressing the north flank of Mount Katmai, are nearly as level as when they accumulated on the bottom of the seafloor.

The first time I reached the caldera in 2011, I stuck to the base of the cleaver, following the margin of the glacier to the west while hugging the exposed rock and glacial till until I needed to step onto the glacier leading to the caldera rim. This time while looking to avoid glacial travel as much as possible—dying alone, trapped in a crevasse seems like a horrible way to go—I chose a slightly more direct route up a steep ash and snow-covered slope slightly east of the main glacier. The sun had yet to soften the frozen snow as I ascended. I couldn’t kick sufficient steps into the crust, which forced me to avoid the steepest snowfields where I felt the risk of falling was too great. This turned into the diciest part of the route and was the one place that I wished I carried an ice axe.

View of hummocky landscape created by ash and pumice covered glaciers at the foot of mountains hidden in clouds. Blue line near center represents route.

I explored the termini of the Knife Creek Glaciers the day before my ascent to the caldera, partly to scout a way through the badlands. My approximate route through a corner of the Knife Creek Glaciers is shown in blue. The view looks east toward the caldera.

At the top of this slope, I reached a bench where the gradient lessened in steepness, kept me temporarily off the glacier, and away from areas prone to rock fall. From here, it was a simple task of avoiding the steep sidewalls prone to sodden late spring avalanches and the center of the glacier where crevasses are more likely to open in June. Not a single cloud hung in the sky, the air was dead calm, and the caldera was only two miles away.

view of mountains with vast snowfields with some small pumice-covered areas in fore and middle ground

The final two miles leading to the caldera

When the 1912 eruption began, Mount Katmai was a triple-peaked and glacially clad 7,600-foot tall volcano. Around midnight on June 7, 1912—in the midst of eruption’s most violent outbursts—Mount Katmai began to collapse. Over the next twenty-four hours, the summit fell inward, generating fourteen earthquakes between magnitudes 6 and 7.

No one witnessed the collapse. Thick ash replaced daylight with an inky blackness across the region. Not until the eruption ceased and skies cleared on June 9 could anyone see that the mountain had lost its top. Because Mount Katmai collapsed, for decades people considered it to be the source of the eruption. In a sense it is, but not from the perspective of explosiveness. Careful study of the eruption’s fallout and pyroclastic flow deposits in the Valley of Ten Thousand Smokes revealed relatively little originated from Mount Katmai. Instead, the vent that opened at Novarupta siphoned away its magma. Perhaps not coincidentally, the elevation of the caldera floor and Novarupta are nearly the same.

Human eyes would not look into the caldera until Robert Griggs and his expedition team slogged their way to the rim from the Pacific coast in 1916. While I enjoyed the advantage of ascending on clear snow with stable footing along with the fore-knowledge of how to get to the rim, Griggs clawed up the volcano’s still muddied and pumice-covered southern slopes, all-the-while pioneering his route, not quite knowing what he’d see or what challenges he’d face until he got there.

When Griggs reached the unstable and knife-edge caldera rim caldera, he found glaciers cleaved flush with the precipitous walls where several thousand feet of mountain once stood. Peering into the gaping earth, Griggs had difficulty comprehending the caldera’s scale, and he stared amazed at a horseshoe-shaped island of lava in a milky, robin-egg-blue lake deep within the bowels of the volcano.

panoramic black and white photo of volcanic caldera.

Jasper Sayer took this remarkable photograph of the Mount Katmai caldera in 1919. It had been seen for the first time only three years prior. I reached the caldera on the opposite side from this photo, near the low point in the rim at left.

From the sight lines along my route, the terrain provides no hint the caldera exists. Although the route’s gradient lessened the closer I got to the rim, the caldera appeared in sudden and spectacular fashion.

panorama view of Mount Katmai caldera on clear sunny day

During a 2011 ascent here, I was forced to retreat within 15 minutes by howling winds, a cloud ceiling which allowed on the scantest of peeks into the bowl, and the threat of snow. On this day though, I sat on the rim for more than two hours, attempting to embed the scene into memory. I couldn’t help but consider how ephemeral it was. The shallow lake first witnessed by Griggs has grown more than 800 feet deep and continues to rise. New glaciers hug the interior walls and calve small icebergs into the water. I watched avalanches of rock and snow tumble more than a thousand feet from the rim to the lake. Water discharged from hydrothermal vents at the bottom of the lake creates greenish-brown swirls with the deep blue of the lake’s surface.

Like the dozen-plus other volcanoes in Katmai, the mountain will churn with unrest again. Its next eruption is unlikely to be as large and landscape changing as the 1912 event, but Mount Katmai’s potential to unleash the power of the Earth remains ever-present. As I sat on the rim, looking at the hole where a several thousand feet of rock once stood, I enjoyed the long moments of calm, wonderfully alone with a mountain only temporarily at rest.

view of mount katmai caldera with steep snow covered cliffs at right and center
view of mount katmai caldera with steep snow covered cliffs at left and center

To learn more about the Valley of Ten Thousand Smokes, read Robert Grigg’s 1922 book about its discovery and exploration. Volcanologists Wes Hildreth and Judy Fierstein authored the authoritative text on the eruption’s geology in The Novarupta-Katmai Eruption of 1912—Largest Eruption Eruption of the 20th Century Centennial Perspectives. Lastly, I devote two chapters in my forthcoming book, The Bears of Brooks Falls: Life and Survival on Alaska’s Brooks River, on the 1912 Novarupta-Katmai eruption’s significance to the region and the creation of Katmai National Park. Look for The Bears of Brooks Falls late this year via Countryman Press.

A Step to Protect Brooks River’s Bears

Each year, the National Park Service in Alaska reviews compendiums for park areas and provides the public with an opportunity to comment on proposed changes or suggest changes. This year, Katmai National Park is proposing a change to its compendium that will give staff greater flexibility when managing the Brooks River area. If you value the river’s wildlife and the bear-watching experience at Brooks River, whether in person or through explore.org’s bearcams, then please support this change.

Visitation at Brooks Camp has skyrocketed to unprecedented levels during the last several years. In 2015, the last full summer I spent as a ranger at Brooks Camp, approximately 9,300 people attended the NPS bear orientation. In 2016, the number of orientations climbed to 10,900. By 2018, the number had grown to 12,500 and in 2019 it reached over 14,000, the highest visitation every recorded at Brooks River. This change may not seem like much (Yellowstone’s Old Faithful Visitor Center often receives over 10,000 people per day in summer). However, the Brooks River corridor is quite small. The river itself is only 1.5 miles long and during the busiest days in July over 500 people and a few dozen brown bears attempt to share its space. The increase in visitation and unrestricted access to the river has created an untenable situation that taxes park staff, facilities, the experience, and the bears’ ability to tolerate and adapt.

graph showing number of people attending bear orientations (y axis) by year (x axis). The number of orientations has doubled since the 2000s.

Attendance to mandatory bear safety orientations can be used as a proxy for overall visitation to Brooks Camp. In the last ten years, the number of people attending the orientations has doubled.

Related: Bears and Humans at Brooks River

Brooks River is a unique place within America’s national parks. In a landscape home to more bears than people, it is Katmai National Park’s most famous bear watching destination. However, it is perhaps the only area in Alaska that is actively managed as a bear-viewing destination yet has no restrictions on access. No permits or guides are required to visit. There is no limit to how many people can visit each day and almost no restrictions on where you can go when you get there. Arriving visitors are required to attend a mandatory bear safety talk that outlines the proper and expected behavior. After that though, you are largely free do go about your business. To help manage the situation, the National Park Service has proposed this change to Katmai’s compendium.

The Superintendent may prohibit activities, impose restrictions or require permits within the Brooks Camp Developed Area. Information on closures and restrictions will be available in the park visitor center. Violating [Brooks Camp Developed Area] closures or restrictions is prohibited.

The NPS lists several reasons for the proposed change.

  • High visitation and improper behavior by people has negatively impacted bears along the river corridor.
  • The park has received more complaints and concerns from the public regarding bear-human interactions.
  • Bears are changing how they use the river, so current closures are becoming increasingly inadequate.
  • Visitation has increased dramatically over the last several years.
  • To better manage the river corridor, the park needs more flexible management tools.

While the proposed change is no panacea for the challenges facing park staff at Brooks River, it can provide an important tool to manage changing situations. For example, it hypothetically allows the NPS to extend the closure around Brooks Falls beyond August 15 or even restrict human access in the lower river area when bear activity is high.

Quite often, proposals for greater restrictions and regulations in national parks attract more opposition than support, especially if the change has the potential to impact public access or business interests. Now though, we have the opportunity to let the NPS know this change is worthwhile and necessary.

Portions of Katmai’s bear population are equally sensitive to human disturbance as the grizzlies in Yellowstone, yet the only area in Katmai where people cannot venture is the immediate area surrounding Brooks Falls, and then only from June 15 to August 15. Since I came to discover Brooks River for myself in 2007, protections for bears have slowly eroded. In the face of skyrocketing visitation, the NPS has proposed a positive step to protect bears and the bear-watching experience. So please send the park a comment expressing your support for the change. Here’s an example to get you started (feel free to customize it as you see fit). You can download a copy of the proposed changes and submit comments on the NPS’s project website. The comment period is open through February 15, 2020.

PS: If you plan to visit Brooks Camp this summer or in the future, please consider subscribing to the Brooks River Pledge. It’s a personal pledge between yourself and Brooks River with the goal to emphasize respect for the bears’ space as well as ways to continue to have a high quality bear viewing experience.

Fat Bear Week 2019 Endorsement

Avoiding the news when your job is internet-based is like avoiding the flu when your entire household is infected. So, try as I might, I keep stumbling upon headlines about upcoming presidential primary elections. The big question on the minds of pundits seems to be, “Will people choose the candidate who best represents their values or the one who they think is most electable?”

As a certified bearcam aficionado and well-known Katmai National Park pundit, I am pleased to announce that I have do not have that issue, at least not for the upcoming “election” called Fat Bear Week. My candidate isn’t a compromise between values and electability. He’s the real deal, the one, the only, the titanic bear known as 747. He deserves your vote.

silhouette of fat bear sitting in river

Don’t you call me pudgy, portly, or stout. Just now tell me once again, who’s fat? (NPS photo of bear 747 by N. Boak)

Seven-four-seven is a giant among bears, an adult male in the prime of his life who uses his size to dominate access to his preferred fishing spots in the jacuzzi and the far pool. His experience and skill pay off each fall, supplying 747 with the substantial fat reserves necessary to survive winter hibernation without eating or drinking.

To get this fat, you need to catch and eat a lot of salmon. Adult brown bears on Kodiak Island consume can consume an incredible 6,146 pounds (2,788 kg) of salmon per bear per year! Given 747’s excellent fishing skills and ability to routinely access the most productive fishing locations at Brooks Falls, I have no doubt his salmon consumption is on par with the biggest Kodiak bears. Stuck in his own version of “feed”-back loop, 747 gets fatter and fatter until it’s time to enter the den. (And, no bears probably can’t get too fat.)

If you don’t believe me about 747’s qualifications, believe the Internet, always an impartial repository of truth and honesty. In 2017, I recorded a video of 747 in all his epic fatness. If anything can be gleaned from viewer comments (and of course we know that YouTube comments represent the highest form of public discourse), 747 is an extra THICC absolute unit who is ready to hibernate through two winters.

The people have spoken.

At Brooks Falls, 747 remains quite dominant and can often access any fishing spot he chooses, which is not surprising given his size. Adult males typically rank at the top of the bear hierarchy. Even so, 747 still faces competition, in real life and in Fat Bear Week. This summer, I was awestruck watching 747 clash with another adult male, 68, in an intense fight.

 

Sixty-eight emerged victorious in the battle, not only securing access to a preferred fishing spot at Brooks Falls but also assuring his dominance over 747. Bloodied from the fight, 747 left the falls area almost immediately and I thought I might not see him for the rest of the evening.

bear standing in water with some blood dripping from his lower lip

747 bleeds from the mouth after his fight with 68 on July 2, 2019.

Within an hour or so, he returned and began fishing like nothing happened. When you only have a few months to prepare for winter hibernation, there’s little time to waste.

Like so many things in life, 747’s Fat Bear Week victory is not guaranteed. My 2017 and 2018 endorsements for 747 were followed by his sound defeat. This year, his competition is just as fat if not fatter.

GIF of bear sitting upright and scratching an itch with her left front paw

Dear Holly,

Game on. See you in the Fat Bear Week finale!

Sincerely,
747’s Campaign Manager

Your Fat Bear Week vote can be based on any number of factors. You can consider a bear’s annual overall growth like that experienced by cubs and subadult bears. Perhaps you want to weight your vote toward bears with extenuating circumstances such as a mother’s cost of raising cubs or the additional challenges older bears face as they age. No matter what though, 747 once again offers you, the astute Fat Bear Week voter, the opportunity to support a bear who is both the fattest and the largest, two traits that are not mutually exclusive.

Complete your civic duty and vote for Brooks River’s fattest bear from October 2 – 8 on Katmai National Park and Preserve’s Facebook page. Look for the head-to-head Fat Bear Week matchups. The bear whose photo receives the most “likes” advances to the next round, until one bear is crowned fattest bear on Fat Bear Tuesday, October 8. Don’t forget to watch Katmai’s fattest bears every day on explore.org.

Fat Bear Week 2019 Bracket.jpg

My Live Bearcam Broadcasts in 2018

This was a busy year on the bearcams, courtesy of explore.org and Katmai National Park. We hosted more live broadcasts this  year than any other year since the bearcams first went live in 2012.

During play-by-play broadcasts Katmai rangers and myself narrated the Brooks River’s wildlife activity, much like broadcasters for sporting event (although the lives of brown bears and salmon is no game). We never knew what might happen during a play-by-play. Watching the prolonged posturing between two of Brooks River’s largest adult males, 856 and 32 Chunk, on July 12 and integrating the ranger’s radio traffic into the September 17th broadcast are two of my favorite play-by-play moments.

The other broadcasts, live chats, typically focused on a specific topic such as bear fishing styles, hibernation, and bear research at Brooks River. Rangers Andrew LaValle and Russ Taylor from Katmai joined me as frequent co-hosts for live chats and I was also fortunate enough to speak with many special guests. Perhaps the most memorable moment from these broadcasts occurred when bear 132 and her spring cub almost stepped on Ranger Andrew and I during our Katmai centennial live chat on September 24.

If you enjoy these, then please watch many other broadcasts hosted by Katmai National Park rangers and staff on explore.org’s education channel on YouTube.

 

Stuff I wrote in 2018

I was busy on a keyboard this year, even though there were long gaps between posts on this site. In case you missed them, here are the posts that I wrote for explore.org in 2018. They are listed in the order they were posted. My personal favorites include “How does a bear family breakup,” “How many salmon will a bear eat,” “Bearcam live chat surprise,” and “Living with Bears in Churchill.”

  • Brooks River Bear Mating Season: In June, food isn’t the only thing on a bear’s mind.
  • 2018 Bearcam Stories: 503: Emancipated from his adopted mom in the spring of 2016, bear 503, also known as Cubadult, has quickly grown into an energetic and often playful young adult.
  • Early June at Brooks Falls:  Standing at the falls from early to mid June is an exercise in patience and an opportunity to reflect on the changes soon to come.
  • 2018 Bearcam Stories: The Elders of Brooks River: Their longevity of Brooks River’s oldest bears demonstrates a level of individual success few bears achieve.
  • The Mouth of Brooks River: The lower river cams provide expansive views, colorful sunrises and sunsets, as well as the opportunity to see many yearly and seasonal changes.
  • What to Look for 2018: The Bear Hierarchy: Watching the ebb and flow of the hierarchy allows us to at least partly understand the conflict and challenges faced by bears.
  • Bear 856: On Top Again: Bear 856 appears to be big enough and healthy enough to show the river’s other adult male bears he’s ready to compete once again.
  • Death of a Bear Cub at Brooks River: As the smallest and most vulnerable of all bears, first year cubs (also called spring cubs or cubs-of-the-year) face significant risks and challenges, not the least of which are larger bears.
  • Dumpling Mountain Hike: Rising over 2000 feet above Brooks River, Dumpling Mountain offers anyone a quick escape from the hustle and bustle of Brooks Camp. Each time I hike on it, I get an opportunity to see the land in a new way.
  • Four Cubs for 402 Again: No matter this family’s fate, we can marvel at 402’s determination to follow her maternal instincts in an attempt raise another generation of Brooks River’s bears.
  • How Does a Bear Family Breakup? Until somewhat recently, I stated that 402 had “abandoned” her yearling (now known as 503). While this might be true in a sense, I no longer think that this is an accurate way of describing the event. After reading more about the emancipation process, I’ve come to believe 402 didn’t abandon her yearling in 2014. She emancipated him.
  • How Many Salmon will a Bear Eat? We often observe bears partake in marathon fishing sessions at Brooks Falls, so how much can they eat in a day or season? Quite a lot.
  • Salmon on the Underwater Bearcam: The calmer, deeper water near the outlet of Brooks River provides salmon with a temporary refuge that is relatively safe and costs them little energy.
  • 451 and Her Yearlings: 451 is currently raising her second litter, and it’s easy to see that the family is skinner than many of the other bears on the bearcams.
  • Bearcam Line of Sight: Where are the bearcams and where, specifically, do they look?
  • Brooks Falls Trail: Simply walking to Brooks Falls can be an exciting and memorable experience and allows great opportunities to explore a changing habitat.
  • Mid Summer Change at Brooks River: Are fewer bears at Brooks River a sign of change?
  • An Exceptional August: Regarding bear activity at Brooks River, August 2018 has been exceptional.
  • Fishing By Snorkeling: Efficient and effective, snorkeling is one of the best strategies to scavenge fish.
  • Can a Bear be Too Fat? When you see bears whose stomachs appear to drag on the ground, one wonders if a bear can grow too fat for its own good.
  • Bearcam Live Chat Surprise: “This being a live broadcast it’s entirely possible…a bear could walk through the screen at any time. So if we have to exit or end the broadcast abruptly that’s probably why.”
  • Fat Bear Week Quarterfinal Preview: The competition just keeps getting bigger.
  • Mike Fitz’s Favorite Bearcam Moments of 2018: Here are a few of my favorite bear cam moments for 2018.
  • Evidence of Rapid Change in Katmai: the Ukak and Savonoski Rivers spill across a broad, 1.5-mile wide delta. In a landscape often defined by change, this is one of the most dynamic places in Katmai National Park.
  • 2018’s Top Ten Bearcam Moments: the people have spoken! Bearcam viewers have chosen the top ten bearcam moments of 2018. Each moment is unique and significant for a different reason.
  • Living with Bears in Churchill: The confluence of bears and people in this remote community has created a special set of challenges, which can only be met through the town’s willingness to tolerate the largest four-legged predator on Earth.

Vote on Climate

In my last post, I explored the origins of an alpine lake in North Cascades. The news cycle was especially terrible the day I wrote it, so I decided to leave out details about the causes and consequences of glacial retreat in North Cascades. But honestly, the causes and consequences are too great to ignore. It is no small irony that my insight and enjoyment into the formation of an alpine lake was inadvertently provided by people through human-caused climate change.

All glaciers in North Cascades are retreating and they’ve collectively lost over 50% of their mass during the last 100 years. This is directly due to a warming climate, a product of burning fossil fuels like coal and oil.

before and after photos of glacier.

Banded Glacier in 1960 (left) and 2016 (right) in North Cascades National Park.

Unless you’ve been living under one of those glaciers for the past century, you might’ve heard there’s an election next week and voting has begun in many states. While casting our votes, we have an opportunity to elect representatives who will work to mitigate climate change. But, we shouldn’t vote to combat climate change just because glaciers are receding in North Cascades National Park.

We should act on climate, because glacial melt water moderates summertime drought. Millions of people depend on glaciers for drinking water.

We should act on climate to lessen the risk from extreme weather events like drought, hurricanes, floods, and heat waves.

We should act on climate to ensure supplies of fresh water are not overly taxed by humanity’s increasing demands. Who wants reliable access to clean fresh water? All of us.

We should act on climate to help reduce the spread of invasive species, many of which are finding easier footholds where ecosystems are already stressed and fragmented.

We should act on climate to prevent the loss of arctic sea ice, a habitat that helps cool the planet by reflecting sunlight into space, forms the basis of a complex polar food web, and is one necessary for the survival of polar bears.

We should act on climate so coastlines aren’t flooded by sea level rise.

We should act on climate to mitigate ocean acidification, which can impact marine food chains. A lot of us eat seafood and even if we don’t, we like animals that eat seafood (whales, bears, etc.). What would Katmai National Park, my favorite place, be without abundant salmon? An impoverished place, that’s what.

I could go on, but I think you get the point.

We have a moral responsibility to stave off the worst climate change impacts, because this is a human-caused issue. Collectively we can do it, but we have to take the threat seriously. We, as a nation, didn’t vote to combat climate change during the 2016 election. Thankfully, we have another chance now, but time is running out to slow and eventually halt what is one of the most pressing issues facing humanity. That’s why I’m voting for initiatives to mitigate climate change and only for candidates who take climate change seriously.

photo of Washington State ballot showing yes selected for Initiative 1631

In Washington, Initiative 1631 would authorize the first carbon tax in the U.S. This is my ballot.

I’ve been fortunate enough in my life to explore active glacial environments in many parts of North America. In Katmai, I’ve walked on pumice-covered glaciers to reach volcanic calderas, numbed my feet in icy glacial runoff, and eaten freshly calved ice (if you’re wondering, it was clean tasting but a little gritty). In the North Cascades I explored the margins of the region’s still active ice. To find an advancing glacier in modern times, however, is rare. Melting glaciers are one of our most conspicuous symbols of global warming.

Glaciers have come and gone in the past, of course. I grew up in a region of Pennsylvania where Ice Age glaciers terminated their last advance, leaving behind eskers and sand quarries. I lived near Lake Chelan, a remarkable inland fjord carved by glaciers. Katmai was also completely overrun by ice. Modern glacial retreat is different though, because we’re the primary cause. Climate change isn’t a hoax or some deep-state conspiracy. It’s real, it’s here, and humans are causing it. There is no scientifically plausible alternative theory that explains the changes to Earth’s climate observed since the Industrial Revolution.

I still find beauty in the ice, but each time I see a glacier I also am reminded of one of Aldo Leopold’s many maxims,

“One of the penalties of an ecological education is that one lives alone in a world of wounds. An ecologist must either harden his shell and make believe that the consequences of science are none of his business, or he must be the doctor who sees the marks of death in a community that believes itself well and does not want to be told otherwise.”

The community is not well, because we’ve wounded it. Let’s step up and act. When you vote, only vote for those who take climate change seriously and, more importantly, will actively work to reduce its impact. The status quo got us here, but the status quo is no longer good enough.

Fat Bear Week 2018 Endorsement

Last October I wrote, “There are small and fat bears, old and fat bears, young and fat bears, and just plain fat bears. But none, NONE I say, are as fat as 747.” A year later, 747 continues to demonstrate his survival skills and success at Brooks River. He’s big enough and fat enough to once again earn my official endorsement for Fat Bear Week 2018. 747 is titanic, a giant among bears.

GIF of large, dark brown bear walking down a steep hill

Bear 747 is an adult male in the prime of his life. First identified as a subadult bear in 2004, he’s matured into the largest bear I’ve ever seen.

 

But don’t just take my word for it. Bear 747 is endorsed by several of his competitors at Brooks River.

bear lying on ground

“Look, we’re all fat right now, but no one is as fat as 747. Seriously, his belly nearly drags on the ground. Even I never achieved that level of pudge. “ Bear 410

profile of bear walking along edge of river

“I keep my distance from him because I’m concerned he’ll roll on top of me.” Bear 68

402_07062016

“I’m still in awe of his size. Can he even dig a den big enough to fit within?” Bear 402.

bear with blond ears and blond coat standing in water

“Even though I’m in the Fat Bear Week bracket, I still might vote for 747. It’s the logical vote. He probably weighs at least three times as much as me.” Bear 719

profile of brown bear standing on edge of waterfall

“747 is a role model of fat bear success. I hope to be as fat as him one day.” Bear 503

bear sitting in water below waterfall

“I’m too hungry to comment.” Bear 480 Otis.

Many people who have observed 747 closely also agree with the endorsement.

bear lying in water facing photographer

“He’s all business—fishing and eating. Nobody gets fat like 747.” Jeanne R., former Katmai National Park ranger.

Too much fat is unhealthy for humans, but fat is essential to the survival of brown bears. It is a savings account against famine. Without ample fat, bears do not survive hibernation. In spring, often a season of starvation for bears, females with cubs will metabolize fat into milk to nurse their growing cubs, and adult males will use their fat to fuel their pursuit of mates.

747 won’t be rearing any cubs next spring as male brown bears play no role in raising offspring. During a season when almost no high calorie foods are available to bears, 747 will use his fat to roam the landscape for mates instead.

Other bears might be more charismatic or tug on your heartstrings, but 747 truly is a giant among Brooks River bears. He deserves your vote for Fat Bear Week 2018.

Katmai Fat Bear Week Bracket 2018 Fitz choices.png

My 2018 Fat Bear Week bracket predictions.

You are encouraged to vote for Brooks River’s fattest bear on Katmai National Park and Preserve’s Facebook page. Starting on Oct. 3, park rangers will post head-to-head matchups between well-known bearcam bears. The bear whose photo receives the most likes will advance to the next round, until one bear is crowned fattest bear on Fat Bear Tuesday, October 9th. Don’t forget to watch Katmai’s fattest bears on bearcam.

 

 

 

A bear, wolves, and a moose carcass

Although they probably inhabit all of Katmai National Park, wolves are infrequent visitors to Brooks River, and seeing a wolf on the bearcam is a noteworthy occasion.

Late one evening at the end of June and about a dozen miles from Brooks River, I was lucky enough to see wolves compete with a bear for food along the middle reaches of Margot Creek.

At the beginning of the video, a blob in the middle of the creek represents the bear as it laid on the moose carcass. Two park rangers observed the same bear on the moose about seven hours before (no one witnessed how the moose died). When presented with a large animal carcass, bears will often bury it and/or sleep directly on it to protect it from other scavengers.

Not long after I started to watch the bear, a wolf emerged from the forest. It circled the bear, perhaps testing how tolerant or defensive the bear might be. Bears are quick, capable of outrunning any human, but they aren’t as fast as a wolf, and wolves know this. Therefore, the wolf was in little danger from the bear as long as it remained wary and stayed out of the bear’s reach. This didn’t stop the bear from charging the wolf several times though (only a few of which I was able to record). Despite the bear’s defensiveness, the wolf was persistent.

low resolution photo of a bear running at a wolf

A bear defends a moose carcass by charging a wolf who approached too closely. Photo courtesy of Anela Ramos.

Soon after the wolf appeared, the bear left the carcass and a second wolf arrived. The wolves didn’t appear to be in sufficient numbers or aggressive enough to chase the bear away. Perhaps the wolves were enough of an annoyance that the bear was unable to rest or the bear could’ve been chilled by lying on the carcass in the creek for several hours. Whatever the reason, after the bear left for good the two wolves quickly began to gorge on the moose. They focused their efforts on the moose’s abdomen, thoroughly eviscerating it within fifteen minutes.

grainy photo of two wolves eating a moose carcass in a creek

Two wolves tear into a moose carcass soon after a brown bear left it unattended. Photo courtesy of Anela Ramos.

Shortly afterward, stomachs bulging with moose entrails and meat (wolves can eat over 20 pounds of food in a single feeding session), the wolves sauntered into the forest.

Events like this happen in many places where wolves and bears share habitat, but in Katmai it might be more intense in spring and early summer before spawning salmon become abundant across the ecosystem. Bears often steal the show at Katmai, but wolves also prowl the landscape, following their own strategies for survival and sometimes competing directly with bears for food.

Return to Bearcam 2018

As many readers of this blog are aware, one of my favorite places in the world is Brooks River in Katmai National Park. There, about 300 miles southwest of Anchorage, Alaska, brown bears and salmon gather to create one of the most iconic scenes in America’s national parks.

many bears standing and fishing near a waterfall

Brooks Falls on a busy evening

 

I’m pleased to announce that through the generosity of explore.org, I’ve received a fellowship to work with Katmai’s bearcams, live streaming webcams of at Brooks River.

In conjunction with Katmai’s park rangers, I’ll write blog posts (which you can read on explore.org and Medium), chat frequently in the bearcam comments, and host live chats and play-by-play style broadcasts. I hope to make time to write about my other explorations on this blog as well.

Bearcam season is almost upon us. Webcam technicians are at Brooks River now, upgrading the webcams for a better live cam streaming experience. The first sockeye salmon should arrive at Brooks River in a matter of days and the bears will arrive soon after. This will be an exciting summer, so please join me here and on bearcam.