Pages

Wednesday, March 21, 2012


Think "Before"
"Prepare" is defined in Webster's Dictionary as "to make ready beforehand for some purpose, use or activity." The inclusion of the word "before" in this definition is not by accident. One way of assuring the success of your trip is to remember the "Rule of Befores".

Listen to a weather forecast before planning a trip. Tell people where you are going and when you'll be back before you leave. While on the trail, drink before you get thirsty, eat before you get hungry. Add a layer of clothes before you get cold; remove a layer of clothes before you get hot. Make camp before you need camp. Find protection from foul weather before it arrives.

By doing these things, you will find yourself always thinking ahead. Think ahead at all times and you will rarely find yourself unprepared.


For more information on backcountry safety, check out the Mountain Rescue Associations public education programs @ http://mra.org/training/public-education



Courage - Commitment - Compassion
     Mountain Rescue Association 

Friday, February 10, 2012

The Public Information Officer in Search and Rescue


What is a Public Information Officer? A Public Information Officer (“PIO”) is a representative of an official organization.  This person serves as a central source of information for release by the department and responds to requests for information by the news media and the community.

In search and rescue operations, the PIO might be a representative of any number of organizations, including: 
1. The local law enforcement entity (frequently the county sheriff or state police); 
2. The local search and rescue organization; or,
3. The regional or state search and rescue organization. 

In any SAR incident, the PIO serves a number of important roles: 
1. Assisting news personnel in covering incidents; 
2. Assisting the news media on an oncall basis; 
3. Preparing and distributing news releases; 
4. Arranging for, and assisting at, news conferences; 
5. Coordinating and authorizing the release of information about victims and incidents; 
6. Assisting in crisis situations within the agency 
7. Coordinating the release of authorized information concerning agency operations 
8. Posting, monitoring and managing the use of Social Media outlets

As you can see from the list above, the primary purpose of the PIO is to provide a central source of information to the media.  At the same time, the PIO serves another equally important role of keeping others in positions of authority and leadership from having to deal with the media while performing their duties. 

It is the role of the PIO to answer the most common questions, those of “who, what, when, where, why, how, how come?”  The PIO then goes on to describe what the various agencies are doing about the situation. Because sharing information with the media can be a difficult job, SAR organizations should be certain to provide necessary and appropriate training for all individuals that might serve in the capacity of PIO. 

Why is a PIO Important? 
The public demands, and indeed deserves, to be made aware of the circumstances and events associated with a SAR incident.  This is best accomplished through the media, which has direct and often immediate access to the public. Furthermore, proper public information at a SAR incident will enable the SAR authority to provide preventive SAR education to the public. 

Over the years, some SAR organizations have tried to avoid dealing with the media.  Some have been known to say, “The media NEVER gets it right.”  In fact, by avoiding the media, a SAR entity can rest assured that the media will not get it right.  Only by dealing directly with the media, in all it's forms, can we assure that the story is as close to accurate as possible. 

Who Makes a Good PIO?
First and foremost, a PIO needs to be very knowledgeable in the field of SAR operations.  For this reason, PIO’s should be chosen from among the veterans of a SAR organization.  Some people are natural teachers, and the role of PIO is somewhat a teaching role.  Still, the best teachers are those who are very well trained in the topic. 

In addition to experience, a PIO needs to have the proper balance of humility and self-confidence.  When he media or public see an egocentric rescuer in front of the camera, then the focus becomes the PIO and his/her agency not the message. 

A good PIO has great respect for the media.  Power comes through knowledge – knowledge that is shared, not knowledge that is kept.  The more respect a PIO has for the media, the better s/he will be at communicating the important messages to them. 

When choosing a PIO, any organization should ask who it wants to be the spokesperson for the group.  often, the most well respected individuals in the organization will be good candidates for PIO.  This is because the respect those individuals have gained over time is most often based on the combination of their personality, knowledge and expertise. Purposefully choose your PIO.  Take your time, and choose someone who is polished, professional, humble, and knowledgeable. 

General Guidelines 
It is true that “bad news travels faster than good news.”  Since most SAR incidents involve some bad news for the victims, the media is often quick to respond to our calls. While a SAR team’s PIO should be prepared at any time to respond to media calls regarding an incident, an experienced PIO will know the moment a SAR call is dispatched whether it will attract media attention. 

There is no such thing as a “media circus.”  The media professionals are there to do their job, and it becomes the PIO’s responsibility/opportunity to help them do their job.  A PIO should maintain an attitude of helpfulness at all times.  His/her perspective should always be, “I’m here to help you, and to make sure I get you the information I have.” Some level of excitement and adrenaline should always be present, so the PIO maintains focus.  A lazy or disinterested PIO makes a bad PIO.

Your PIO should also not ignore social media. Frequently, social media streams like Twitter and Facebook are breaking stories well before more traditional media outlets can get on scene. In some cases traditional media organizations like CNN and their iReport site are even "crowdsourcing" news.  Because of the nature of social media, these tools can be used not only to get your message out, but also to see how you message is being understood by the public. As it is two way communication, it can also be used to gather information. 

Consider posting missing person information and mission updates to your team Facebook Page and Twitter feeds but only do so with the authorization of the agency having jurisdiction. Because this can be done "in the moment" and from mobile devices, this can keep the public updated outside of the traditional media cycle.    

We will go more into Social Media for Search and Rescue at the joint MRA / NASAR Conference in June and will follow up with a blog post. 

Stay Safe!

For more information on how to effectively work with the media, check out the Mountain Rescue Associations rescuer education program http://mra.org/images/stories/docs/workingwithmedia.pdf 


Courage - Commitment - Compassion
     Mountain Rescue Association 

Friday, January 27, 2012



Hypothermia...The Most Common Killer of Backcountry Users 
On February 1, 1989, the temperature in Butte, Montana dropped from 42 degrees to -4 in one hour. Regardless of the season, a temperature drop of 30-40 degrees Fahrenheit in one hour is not uncommon in the mountains.  Add cold rain and wind and nature has mixed the perfect recipe for hypothermia. 

What is Hypothermia? 
Hypothermia is the rapid, progressive mental and physical collapse accompanying the chilling of the inner core of the body.  It is caused by exposure to cold, aggravated by wet, wind and exhaustion. Hypothermia has killed more unprepared backcountry users than any other malady.  In fact, the state with the most reported cases of hypothermia is, believe it or not, Florida!  The reason is simple. Floridians are generally unprepared for cold weather. 

There are a number of ways to avoid hypothermia.  The trick to staying warm is to gain more calories than you lose.  The body can burn as little as 50 calories per hour while sleeping or more than 1,000 an hour during heavy work.  Just as the body constantly produces heat, it constantly loses it.   

Your body may burn over 50% more fuel in winter than it would in summer.  This is because you are inhaling cold air, warming it and saturating it with water vapor.  In fact, as much as one-third of your body-heat loss can occur through breathing.  Breathing through a scarf or balaclava may help by "pre-heating" the inspired air.  The body also loses heat by perspiration and its subsequent evaporation from the skin.  In addition, 75% of the body heat can be radiated from an unprotected head, since the blood vessels in the scalp lie close to the 
skin. 

Creating Body Heat Clothing and shelter can only conserve body-heat, they can't create it.  Liquids and food are the only "internal" source of heat creation for the body.  This is because heat is produced in the body by chemical reactions through the metabolism of food, mainly oxidation of carbohydrates.  Muscular activity is a second source of heat, but uses food energy to generate the heat. 

The Body's Reaction to Cold 
The body's first reaction to cold is to shiver. Shivering is the first sign of hypothermia and is the body's way of forcing an isometric contraction and triggering a stored glycogen "dump" from the liver.  It is the body's attempt to generate heat by rapidly and rhythmically contracting muscles. Despite the fact that shivering is fatiguing, it generally helps keep us warm.  It diminishes with oxygen deficiency, breathing of carbon  monoxide or the taking of aspirin or alcohol.  The body's ability to maintain warmth is depressed by the lack of water, lack of food, fatigue and shock. After shivering stops, hypothermic victims are confused into thinking they are feeling warmer. THEY ARE NOT.  They are dying. 

Problems Which Increase Hypothermia Dangers 
Constipation retards efficient metabolism of food and reduces energy levels.  This is a dangerous situation in the winter, as the body can no longer take advantage of the energy provided by the "fuel" ingested. Despite what grandmother told you on those cold Wisconsin evenings, alcohol reduces the body's ability to fight cold.  It dilates peripheral blood vessels, blocking vasoconstriction and allowing warm blood to exit the body's core.  In addition, the alcohol may actually make the victim feel warm and more competent. The low temperatures will increase the intoxication because brain cell membranes are more fluid as a result of the increased metabolism.  Smoking or chewing tobacco constricts peripheral vessels, reducing circulation necessary to keep the skin warm.  Aspirin also dilates the vessels.  Such conditions are conducive to frostbite and hypothermia. In addition, sedatives, antidepressants and neurological problems common in the 
elderly will all increase the risk of hypothermia. 

Hypothermia is a killer in summer as well as winter.  It is more often triggered by a combination of wind, wet and cold than by cold alone. In fact, just plain dry cold, even at extremes of -30 degrees, is far more manageable and far more pleasant than 20-degree weather with wet snow and rain falling and a harsh wind blowing.  I'll take the 30 below any day. 

The Hypothermia Lab in Duluth Minnesota has studied this phenomenon for over a decade.  The lab discovered that the human body can adjust its metabolism to adapt to the cold.  Studies showed that Eskimos respond to cooling with an almost instant metabolic leap and with skin temperatures that remain remarkably high.  The "Ama", Korean pearl divers who once dived naked into icy waters in search of treasure, had high basal metabolic rates, more efficient tissue insulation and a higher threshold of tolerance before the onset of shivering.  One generation after they had started using wet-suits, they had completely lost their specialized responses to the cold. 

Hypothermia and the Mind 
The Hypothermia Lab also found that circulation can be increased by mind-power.  Subjects of experiments who thought about how much they wanted to get out of the cold suffered rapidly falling body temperatures.  On the other hand, shivering subjects, directed to perform a mental arithmetic task, stopped shivering for short periods.  In addition, when people get anxious, they have more problems with temperature 
regulation.   

One of hypothermia's strangest manifestations is "paradoxical undressing." People suffering severe hypothermia are often observed throwing off their clothes, as if they felt they were burning up.  This is believed to be because the hypothermic victim's body, which has been vasoconstricted to maintain core heat, may abruptly vasodilate, allowing warm blood to pump briefly through the body's peripheral areas. To the hypothermic victim, who is already mentally foggy, the vasodilation may produce a sense of extreme warmth. In addition, chemical changes occur in the body that can make the situation more dangerous.  First, epinephrine (adrenaline) is released into the bloodstream, which increases the heart rate.  This is healthy, since it increases the metabolism.  Other chemical changes, however, can cause hypothermic victims to experience vivid hallucinations very similar to those reported by schizophrenics.  This is believed to be caused by increased dopamine in the blood.  In addition, researchers have found that spinal and cerebral neurons become hypersensitive when they are cooled just three or four degrees below normal.  This can lead to neural misfiring and to seeing things that just aren't there. 

Believe the signs, not the victim.  
Team members should monitor each other carefully, even in temperatures of 50 degrees.  Any early sign of hypothermia is a serious warning. Take immediate action to correct the situation before it is too late. Most cases of hypothermia develop in temperatures between 30 and 50 degrees Fahrenheit.  Many novice backcountry users simply don't believe such temperatures are dangerous.  They fatally underestimate the dangers of being wet and/or poorly clothed at such temperatures. 

Environmental Conditions Contributing to Hypothermia 
When the body is wet, the evaporation of moisture from the skin has a very rapid cooling effect that can be extremely dangerous.  Water conducts heat 25 times faster than air.  Therefore, heat is lost much more quickly if evaporation is occurring.  A wet backcountry user must always change quickly into extra dry clothing as soon as possible.  Staying wet is an open invitation to the dangers of hypothermia. It is equally important to protect yourself from your own sweat.  Working up a sweat on the trail will result in wet clothes by the time a final destination or resting place is reached.  Wet clothes will chill the body significantly, especially in conditions of high wind where evaporation takes place much more quickly. 

The Body's Reaction to Hypothermia 
Mother often said and (for once) she was right:  "If you want to keep your feet warm, wear a hat."  Up to 75% of heat loss is through your head and neck, since the blood vessels are close to the surface.  If the head, or any other body part, is exposed to cold, the body chills and "shunting" can result.  When this happens, circulation to the extremities is sacrificed to assure that the remaining body heat is reserved for vital internal organs.  The result is that the hands and feet receive less warm blood. Shunting occurs as a result of vasoconstriction. Vasoconstriction cranks up your blood pressure as you chill.  As a result, cold can be dangerous for people with heart disease. 

The key to avoiding this dangerous situation is to be brave (and smart) enough to give up reaching the peak when the first signs of hypothermia present themselves. 

Have fun and stay safe out there!

For more information on backcountry safety, check out the Mountain Rescue Associations public education programs @ http://mra.org/training/public-education

Courage - Commitment - Compassion
     Mountain Rescue Association 

Friday, January 6, 2012



Avalanche!!!! The Snowpack Variable 


Snowpack is the last variable that we will use for clues.  By combining the clues you observe, identify and feel from the snowpack, a decision should easily be made whether or not the snow is unstable and has potential to slide. Some of the signs of avalanche are obvious.  The following clues are direct indications of instability in the snowpack: 


Recent Avalanche Activity 
Again, recent avalanche activity is the best indicator of dangerous slopes, especially when it is on slopes of similar aspect and steepness.  In other words, if you see the debris from a recent avalanche, know that there is danger of additional avalanches on similar slopes. 


                                              A bad day on the snow 

Recent Wind-Loading  
Recent wind-loading is another indicator of avalanche danger.  Smooth "pillows" and cornices as well as snow plumes of the ridge tops are indicators of wind-transported snow.  This means increased stress is being exerted on the snowpack due to the addition of the wind deposited snow.  Furthermore, wind deposited crystals develop dangerous "wind slabs," since this type of crystal is subject to numerous collisions while the snow is wind-blown. 


Hollow Sounds 
You must use your ears as you evaluate avalanche hazard.  "Drum-like" or "whumpf" sounds that occur under your feet indicate unstable slab conditions.  Also, pay attention to distinctive settling sounds; feeling the snow settle or drop are clues of an unstable layer of snow...indicating a dangerous avalanche condition. 


Shooting Cracks 
Look closely at the terrain you wish to cross.  Cracks in the snow around you are an excellent indicator of avalanche danger, especially if they are occurring around you as you move across the snowpack. You should not only avoid the slope where you see or produce cracks, but also any slopes with similar profile and/or orientation. 


Snow Stability Tests 
Through additional training, you can learn to recognize the weaknesses in the snowpack by evaluating a cut-away of the snow layers.  For now, just remember that avalanches occur when a weak layer in the snowpack fails.  Your ability to recognize these weaknesses will help you make an educated decision regarding safe backcountry travel. 


Conclusion 
In summary, by looking, listening and feeling you should be able to recognize, evaluate and avoid avalanche hazards that you may encounter on your next backcountry trip.  You must be thinking avalanche whenever you are on or near slopes, regardless of the slope size and time of year.  By always thinking avalanche you will be much more observant, you will gather more information from clues, and you will become a better decision-maker


For more information on avalanche safety check out the Mountain Rescue Associations public education program @ http://mra.org/images/stories/training/Avalanche.pdf as well as our Backcountry Skiing & Riding Safety Video  


Courage - Commitment - Compassion
     Mountain Rescue Association 

Tuesday, January 3, 2012

Avalanche!!!! The Terrain Variable 



Learning to identify avalanche terrain is most important in recognizing and evaluating avalanche hazard.  It's asy to recognize where avalanches are common and where they are not. 


Slope Steepness 
The steepness of a slope is a key factor in determining avalanche danger.  It is a common misconception that avalanches occur on steep slopes.  The fact is that most avalanches occur on slopes of 30 to 45 degrees.  It is within this range of steepness that the balance between the strength of the layers of snow and the stress of gravity is most critical.  Steeper slopes tend not to hold a significant amount of snow due to gravity.  


Slopes of less than 30 degrees may not be as prone to slide, but may be as dangerous in the right conditions especially in the spring when wet avalanches occur. Unfortunately, 30 to 45 degrees also provides the most challenging ski terrain. 


Remember, too, that short slopes may be as dangerous as long ones.


For a lesson on how to use an Inclinometer for your slope steepness check out this post from Skiing the Backcountry http://www.skiingthebackcountry.com/skiing-resources/how_to_use_inclinometer


Slope Orientation 
The orientation of a slope is also an important factor.  By "orientation," we mean whether the slope is having snow blown onto it or blown off from it.  We also mean whether the slope faces north or south.  Leeward slopes, or those drifted by winds, are more dangerous because of the added depth and weight of the snow. North-facing and shaded slopes tend to be more dangerous during the mid-winter periods, mostly because of the colder surface temperatures.  South-facing slopes tend to be more dangerous during spring thaw, specially on a sunny day, due to solar heating and the introduction of water (melting snow on the surface) into the 
snowpack. 


Slope Profile 
We must also evaluate the slope profile.  That is, whether the slope is flat or curved.  Convex slopes are likely to fracture at the bulge.  Concave slopes provide a certain amount of support at the base, though they are still capable of avalanching. 


Be especially cautious around bowl-shaped slopes or those with narrow, deep gullies.  Both of these features help trap blowing snow, especially on the leeward side of the mountain. 


Vegetation 
Vegetation can be a key indication of avalanche hazard.  The first thing to look for is "ground cover."  Large rocks, trees and heavy brush help anchor the snow, at least until they become covered.  Avalanches can start even in the trees, since sparse trees can actually weeken the snow cover.  To be reasonably safe, the trees must be so dense as to make it difficult to maneuver. Equally important, yet often neglected, is knowing what the slope looks like without the snowpack.  If the slope is a grassy hill in the summer, it is more likely to slide due to the lack of anchors. Conversely, if the slope is known to have many large rocks, tree stumps or bushes, it may be more stable.  


This is true only as long as the snowpack is not so deep as to cover these natural anchors. 


Elevation 
What about elevation?  Avalanche danger generally increases with elevation.  Most large avalanche starting zones are above timberline.  This is due to the fact that there is generally a greater snow cover above treeline.  In addition, there are less natural anchors above treeline. 

Our next post will wrap up our series on the variables that help develop a potentially unstable snowcover with a discussion of snowpack. By understanding these variables, backcountry users will have a better chance of predicting avalanche danger.


For more information on avalanche safety check out the Mountain Rescue Associations public education program @ http://mra.org/images/stories/training/Avalanche.pdf as well as our Backcountry Skiing & Riding Safety Video  


Courage - Commitment - Compassion
     Mountain Rescue Association 

Friday, December 9, 2011

Avalanche!!!! The Weather Variable 

The first significant contributing factor is weather.  80% of avalanches occur during or shortly after a storm.  For this reason, the information gathering process must begin BEFORE you leave on your outing.

Before you leave home, gather as much information as possible!  Utilize your local avalanche forecast center's web site and/or recorded avalanche hot line and listen to weather reports on the TV and radio.  The local Ski Patrol may also have information regarding the latest avalanche forecast.

Invest in a commercially sold cross-country trail map if one exists for the area you plan to visit.  Sometimes, dangerous avalanche zones are noted, giving you advance warning of problem areas.

What should you look for when on the trail?  Beware of changing weather patterns, especially unusual changes in wind, snowfall and temperatures.

Storms 
The first thing to look for is storms.  Remember that 80% of avalanches occur during or shortly after a storm, often because of the fact that the existing snowpack cannot support the weight of the new snow, especially if stressed by the added weight of a skier or snowmobiler.

Winds 
You must also be alert to the presence of winds.  Winds of over 15 M.P.H. cause avalanche hazard to increase greatly.  Under these conditions, the wind lifts snow from windward slopes and redeposits it onto leeward slopes.  This produces greater accumulations of heavier, denser snow on these leeward slopes, which stresses the existing snowpack.  Snow plumes off the tops of ridges are a good indication that wind is moving the snow.  Cornices on leeward slopes indicate accumulations of wind-deposited snow.

New Snow 
Snow falling at a rate of one inch per hour or greater increases the avalanche danger as a result of the increased weight.  If a foot or more of fresh snow is deposited at one time, then avalanche danger is often extreme.  Even four inches of fresh snow is dangerous, in conditions of high wind.

Temperature 
Snow remains unstable (or may become less stable) in cold temperatures, due to the temperature difference between the surface of the snow and the surface of the ground.  Once temperatures climb into the range of
20-32 degrees, the snow cover will rapidly stabilize, due to settling.  Temperatures above freezing produce very dangerous conditions, because melting snow introduces water into the snowpack.

Water 
weakens the existing snow crystals and acts as a lubricant in the snowpack.  In other words, temperatures significantly above freezing increase the danger

In our next few posts we will continue to discuss the three main variables that help develop a potentially unstable snowcover: weather, terrain and snowpack. By understanding these variables, backcountry users will have a better chance of predicting avalanche danger.


For more information on avalanche safety check out the Mountain Rescue Associations public education program @ http://mra.org/images/stories/training/Avalanche.pdf as well as our Backcountry Skiing & Riding Safety Video  


Courage - Commitment - Compassion
     Mountain Rescue Association 

Wednesday, November 30, 2011


The "Average" Avalanche

Avalanches come in all shapes and sizes.  The average snow avalanche is 2 to 3 feet deep at the fracture line, about 150 feet wide and will fall about 400 feet in elevation.  That's a slide area bigger than a football field!  What's more impressive is that the average avalanche travels at speeds around 50 M.P.H., a little faster than most of us like to ski!  The average time duration of a slide of this size is less than 30 seconds.  This is the size of avalanche that catches and kills most backcountry travelers.

Avalanches can be much larger...some of the largest reported avalanches have involved complete mountainsides of snow, the area of 20 football fields, having a depth of 10 feet at the fracture line and falling over 1½ miles at speeds well over 100 miles per hour!  As impressive as these avalanches are, generally the smaller ones are the killers.  In fact, 50% of avalanche fatalities are killed in slides of less than 100 feet and people have been killed in slides of less than 40 feet.  The bigger ones almost always release from natural causes and do not involve people unless they happen to be in the wrong place at the wrong time. Artificial triggers, such as snowmobiles or skiers are much more effective at releasing small to medium sized avalanches in shallower snowpack, where the stress caused by their weight is enough to cause the snowpack to fail.

Avalanches are a powerful phenomenon.  In 1969 at a ski hill in Washington, steel chair-lift poles were bent in an avalanche.  In a recent Colorado avalanche, a flashlight inside a glove compartment of a buried automobile was found completely packed with snow.  Larger avalanches possess the force to uproot mature forests and even destroy structures built of concrete. The reason, forces in excess of 15,000 lbs. per square foot.

The fastest recorded avalanche occurred in Japan and was measured to be traveling at speeds in excess of 230 m.p.h.

Avalanches come in two distinctly different types...  “Loose Snow” and “Slab”avalanches.

Loose snow avalanches are a cohesionless mass of snow that start at a point and fan out as they run, forming an inverted "V".  This type of avalanche usually involves small amounts of near-surface snow and is not considered a major threat to people.  Do not lose respect for these slides as they have taken lives.

Slab avalanches, on the other hand, start when a large area of cohesive snow fails and slides down the slope.  There is a well defined fracture line from where the snow broke away.  In addition, there may be angular blocks or chunks of snow in the slide, sometimes larger than a refrigerator.   A slab avalanche can involve a range of snow thickness from just near surface layers to an event that includes the entire snow cover down to the ground.

Slab avalanches are almost always caused by additional stress on the hill, such as a snowmobiler or skier. Since slab avalanches cause nearly all avalanche accidents, it is important to understand the conditions within the snowpack that lead to these slab avalanches

Snowstorms and wind-redistribution cause the snowpack to develop in layers. Once a layer has achieved sufficient cohesive strength, the first prerequisite for a slab avalanche has been established.  Weather will help add the second requirement...  a weak layer.  If a weak layer has developed underneath a strong layer, the perfect recipe for an avalanche exists.  If the weak layer fails, the cohesive strong layer above it will fracture and fall away from the stress. Both ingredients - a cohesive layer of snow and a weak layer below - are necessary for a slab avalanche.

When the strong layer fractures, the crack is estimated to shoot across the snowfield at a speed of over 1000 miles per hour.

In our next few posts we will discuss the three main variables that help develop a potentially unstable snowcover:  weather, terrain and snowpack. By understanding these variables, backcountry users will have a better chance of predicting avalanche danger.


For more information on avalanche safety check out the Mountain Rescue Associations public education program @ http://mra.org/images/stories/training/Avalanche.pdf as well as our Backcountry Skiing & Riding Safety Video  


Courage - Commitment - Compassion
     Mountain Rescue Association