11 - Environmental Emergencies
Download
Report
Transcript 11 - Environmental Emergencies
Environmental Emergencies
Provincial Reciprocity Attainment Program
Environmental Emergencies
A medical emergency caused by or
exacerbated due to exposure to
environmental, terrain, or atmospheric
pressure
Common terms
Thermoregulation
The maintenance of internal body temperature
at or near the set point of 36.5 ºC
Thermogenesis
The regulation of heat production
Thermolysis
Regulation of heat loss
Thermoregulation
Regulatory centre located in posterior
hypothalamus
Central thermoreceptor (stimulated by blood temp)
near anterior hypothalamus, peripheral
thermoreceptors of skin, and some mucous
membranes
Control temperature through vasoconstriction /
vasodilation, perspiration, and increased circulation
to skin
Regulating heat production
Heat is generated through
mechanical, chemical,
metabolic, and endocrine
activities
Mechanical
Shivering
Chemically
Cellular metabolism
Endocrine
Hormone release
Regulating heat production
Cell metabolism
Breathing
Sweating
Arrector pilli (piloerection)
↑ HR
Shunting of blood
Dilation/constriction of
blood vessels
Core shunting
Muscle movement
Fluid intake
↑ food intake
Sleep
ADH release
↑ urination
Catecholamine
release
Regulating heat loss
Heat is naturally lost through
Radiation
Convection
Conduction
Evaporation
Body Temperature
Maintenance
Physiologic responses — controlled by the
brain (involuntary, such as shivering and
vasoconstriction)
Deliberate actions — (such as exerting
yourself or putting on layers of clothing to
retain heat when you stop exercising)
Regulating Heat Loss
Heat is lost from the body to the external
environment through the skin, lungs, and
excretions
The skin is most important in regulating
heat loss
Radiation, conduction, convection, and
evaporation are the major sources of
heat loss
Convection
Happens when air or water with a lower
temperature than the body comes into
contact with the skin and then moves on
You use convection when you blow on
hot food or liquids to cool them
Amount of heat lost depends on the
temperature difference between your
body and the environment, plus the
speed with which the air or water is
moving
Convection
If you are not moving, and the air is still,
you can tolerate a cold environment quite
well
Air in motion takes away a LOT of heat
With air in motion, the amount of heat
lost increases as a square of the wind’s
speed
A breeze of 8 mph (12.8 km/h) will take
away FOUR times as much heat as a
breeze of 4 mph (6.4 km/h)
Convection
Above wind speeds of 30 mph (48
km/h), the point becomes moot,
because the air does not stay in
contact with the body long enough to
be warmed to skin temperature
Convective cooling is much more rapid
in cold water because the amount of
heat needed to warm the water is far
greater than the amount of heat
needed to heat the same volume of air
Conduction
Transfer of heat away from the body to
objects or substances it comes into
contact with
This is the one where grabbing a door
handle with a moist hand at -40º gives
you a chance to stick around...
Stones and ice are good heat
conductors, which is why you get cold
when you sit on them
Conduction
Air conducts heat poorly — still air is an
excellent insulator
Water conductivity is 240 times greater
than that of dry air
The ground is also a good heat
conductor, which is why you need a foam
pad or other insulating barrier under a
sleeping bag if you want to stay warm
overnight
Conduction
Alcohol is an excellent heat conductor
that remains liquid well below the
freezing temperature of water
At very cold temperatures, drinking
alcohol (ethanol) can result in flashfreezing of tissues inside the mouth
If the back of the throat and the
esophagus become frozen this way, the
resulting injury is often lethal
Evaporation
Responsible for 20% - 30% of heat loss
in temperate conditions
About 2/3 of evaporative heat loss takes
place from the skin in thermoneutral
conditions
Remaining evaporative heat loss
happens in the lungs and airway
In cold weather, airway evaporative
heat loss increases as the incoming air
is humidified and warmed
Evaporation
In cold weather, 3 - 4 litres of water per
day are required to humidify inhaled air
1500 - 2000 kilocalories (Cal) of heat are
lost in this way on a cold day
This fluid loss, if not replaced, results in
dehydration, causing a lowered blood
volume and increased risk of developing
hypothermia
Evaporation
Wet clothing enhances heat loss
Sweat-drenched clothing conducts heat
toward surface layers of clothing
Wet outer clothing layers enhance heat
loss to the environment through
evaporation
A combination of sweat-soaked inner
clothing layers and wet outer clothing
can be quite lethal
Radiation
Direct emission or absorption of heat
Heat radiates from the body to the
clothing, then from the clothing to the
environment
The greater the difference between body
and environmental temperatures, the
greater the rate of heat loss
Clothing that adequately controls the
rates of conductive and convective heat
loss will compensate for the radiation
heat loss
Cold / aquatic emergencies
Localized cold injuries
Hypothermia
Hyperthermia
Drowning
Diving Emergencies
Localized cold Injuries
Classifications/Symptoms
A common classification separates localized
cold injury into three categories
Frostnip (the mildest form of cold exposure)
may be treated without loss of tissue
Superficial frostbite
there is at least some minimal tissue loss
Deep frostbite
there is significant tissue loss even with appropriate
therapy
Frost nip
AKA chilblains
The mildest and most common form of localized
cold injury
Fingertips, ears, nose and toes commonly affected,
characterized by numbness, coldness, and pain
without swelling
Re-warming is safe even with friction if sure not
superficial frostbite
Frostbite
A localized injury that results from
environmentally induced freezing of body
tissues
Pathophysiology
Ice tissues form
Vascular abnormalities occur
Cellular injury caused
Increased sensitivity to reoccurrence
Frostbite
Predisposing factors
Peripheral neuropathies
PVD
Alcohol / tobacco use
Inadequate protection
Nutritional deficiencies
Medication administration
PmHx frostbite
Injury / illness / fatigue
Superficial Frostbite
Some freezing of dermal tissue
Initial redness followed by blanching
Diminished tactile sensation
Pain
Deep Frostbite
Freezing of dermal and subcutaneous layers
White appearance
Hard (frozen) to palpation
Loss of sensation
Management ?
Frostbite
Edema and blister formation 24 hours after
frostbite injury in area covered by tightly
fitted boot.
.
Deep
Frostbite
Gangrenous necrosis 6 weeks after frostbite injury
Hypothermia
Hypothermia
Is defined as a core temperature less than 35°C
(95º F).
Most commonly seen in cold climates, but can
develop without exposure to extreme
environmental conditions
May result from:
A decrease in heat production
An increase in heat loss
A combination of these factors
Hypothermia
If left untreated, hypothermia can kill.
Nobody ever froze to death — instead, they died of
hypothermia.
The freezing part came later…
...and only if the temperature of the surrounding
environment was below freezing.
Predisposing Factors
Age
Medical conditions
Prescription and over-the-counter medications
Alcohol or recreational drugs
Previous rate of exertion
Environmental Factors
External environmental factors that may
contribute to a medical emergency
Climate
Season
Weather
Atmospheric pressure
Terrain
Progression
Clinical signs and symptoms may be divided
into three classes:
Mild
core temperature between 34º and 36º C (93.2º
and 96.8º F)
Moderate
core temperature between 30º and 34º C (86º
and 93º F)
Severe
core temperature below 30º C (86 º F)
Clinical Features
Mild (34º and 36º C) - ( pissed off stage )
LOC Withdrawn
Slurred Speech
HR Normal (May increase initially)
BP Normal (May increase initially)
Other Shivering
Clinical Features
Moderate (30º and 34º C) - ( stupid ass stage )
LOC
Confused, sleepy, irrational, Clumsy, Stumbling
HR
Slow and/or weak
May see EKG changes
BP
Decreasing
RR
Bradypnea
Other
Cyanosis
Dilated Pupils
Clinical Features
Severe (below 30º C) - ( I’m going to die
stage )
LOC Stupor to Unconscious
HR Slow (may be irregular), Absent
EKG Changes (high risk)
BP Hypotensive
RR Bradypnea or apnea
Other Cyanosis
Dilated Pupils
EKG Changes
Hypothermia causes characteristic EKG
changes:
T-Wave inversion
PR, QRS, QT intervals may increase
Muscle Tremor Artifact
Arrhythmias
Sinus Brady, AFib, AFlut, AV Block,
PVC’s, VFib, Asystole
Complications
While the risk of complications are low in
healthy people, there are a few to be
aware of
Most of these result from pre-existing
health problems
Pneumonia
Acute pancreatitis
Thromboses
Complications
Pulmonary edema
Acute renal failure due to tubular
necrosis
Increased renal potassium excretion
leading to alkalosis
Hemolysis (breakdown of red blood
cells)
Depressed bone marrow function
Inadequate blood clotting
Low serum phosphorus
Complications
Seizures
Hematuria (blood in the urine)
Myoglobinuria (muscle pigment that
looks like blood in the urine)
Simian deformity of the hand
Temporary adrenal insufficiency
Gastric erosion or ulceration
Stages of Hypothermia
Shivering
Apathy or Decreased Muscle Function
Decreased Level of Consciousness
Decreased Vital Signs
Death
Immersion Hypothermia
In relation to hypothermia, cold water has
two specific threat characteristics:
Extreme thermal conductivity
The specific heat of water
Worsened with saturation of clothing by
water
The body cannot maintain temperature is
water less than 92 degrees F
Immersion Hypothermia
Sudden immersed in cold water causes;
Peripheral vasoconstriction causing
increased BP
Tachycardia due to anxiety
Lethal dysrhythmias often occur, especially
in patients with cardiovascular /
cardioelectrical abnormalities
Immersion Hypothermia
Immersion hyperventilation is the first
risk…
Immersion in cold water initially causes a
breathing pattern of deep, involuntary gasps
Followed by a minute or more of deep, rapid
breaths, with tidal volumes about five times
normal
Drowning often occurs especially in
conjunction with deep immersion or rough
water
Immersion Hypothermia
Hyperventilation causes alkalosis
Alkalosis increases the blood’s pH
Physiologic responses
causes cerebral hypoxia
to
alkalosis
Syncope increases the risk of drowning
Immersion Hypothermia
In 15°C (60°F) water breath can only be
held approx. 1/3 normal increasing the
risk of drowning when submersion
occurs for more than a few seconds
Mammalian diving reflex phenomenon
occurs as a mode of self preservation
Mammalian Diving Reflex
Cold water ( < 68 degrees F ) immersion
causes
Results in apnea, vasoconstriction,
bradycardia and slowed metabolism without
the risk of aspiration
Vascular bed also becomes engorged with
blood in attempt to equalize pressure from
outside the body
Mammalian Diving Reflex
20 - 30 % reduction in heart rate
Complete recovery after 60 min possible
Redistribution of blood flow from the
periphery to the core
Mammalian Diving Reflex
Muscles cool and nerve impulses slow,
causing slow, weak, poorly coordinated
movements
Treading water or swimming much more
difficult
Dysfunction increases as the tissues cool,
causing inability to swim or tread water after
10-15 minutes in 10°C (50°F) water
Immersion Hypothermia
This stage is reached in as little as 5
minutes in icy water
The patient is no longer able to assist in
his or her rescue
In such cases water rescue is imperative
Hypothermia does not cause deaths early in
cold water immersion emergencies
Death results from drowning or cardiac
dysrhythmias
Immersion Hypothermia
After 10-15 minutes of immersion,
shivering is constant and obvious
Core temp cooling has not occurred
Shivering may temporarily prevent heat
loss in dry air, but not in cold water (
remember 240 x )
Core temp fall commonly occurs around
15-20 minutes in cold (50°F (10°C)) water
Immersion Hypothermia
68
59
50
41
32
Water Temperature
ºF
ºC
20
15
10
5
0
Cooling Rate
ºC/hr
0.5
1.5
2.5
4.0
6.0
Non-exercising adults, light clothing, wearing PFDs
Immersion Hypothermia
Once immersed, swimming is a
dangerous choice to make
An average person who can ordinarily swim
well probably will not be able to swim more
than 1 km (.062 mi) in 50°F (10°C) water on a
calm day
People who tread water lose heat about 30%
faster than people holding still while wearing
a PFD
Systemic Heat Related Illness
Hyperthermia
Heat illness results from one of two basic
causes:
Normal thermoregulatory mechanisms
are overwhelmed by environment
Excessive exercise
Failure of the thermoregulatory
mechanisms
Elderly, ill or debilitated
Maintenance of Thermoregulation
Hyperthermic compensation
Increased heat loss
Vasodilatation of skin vessels
Sweating
Decreased heat production
Decreased muscle tone and voluntary
activity
Decreased hormone secretion
Decreased appetite
Heat Illness
Heat Illness can be described by three basic
forms:
Heat Cramps
Heat Exhaustion
Heat Stroke
Classic
Exertional
Heat Cramps
Brief, intermittent, and often severe
muscular cramps or spasms
Believed to be caused primarily by a
rapid loss of salt during profuse sweating
Cramps may worsen
if salts are not replenished
When Ca levels are low
Too much water is drunk by patient
( Na / H2O ratio disruption )
Heat Cramps
Signs and Symptoms
A/O X3
Hot Sweaty Skin
Tachycardia
Normotensive
Normal Body Core Temp (BCT)
Heat Cramps
Treatment
Remove Pt from environment
Remove excess clothing
Replace salt and water if conscious (First
Aid treatment)
1 – 2 tsp of sugar in 1 liter of water
Gatorade et al
If Severe, IV N/S
Heat Exhaustion
A more severe form of heat illness
Mild-to-moderate core temperature elevation
(less than 39ºC)
A relative state of shock
Most commonly associated with:
Profuse sweating
Water and salt deficiencies cause electrolyte
imbalance
Vasomotor response causes inadequate
peripheral and cerebral perfusion from pooling
S / S of Heat Exhaustion
LOC (Irritable, poor judgment, dizziness,
headache)
Pale, Cool, Clammy Skin
Tachycardia
Tachypnea
Cramps
Nausea/Vomiting
Blurred Vision or Dilated pupils
In severe cases may see orthostatic
hypotension and syncope
Treatment of Heat Exhaustion
Remove Pt from environment
Remove excess clothing
Replace salt and water if conscious
Oxygen (100% NRB)
Begin Cooling (Slowly)
IV N/S
Heat Stroke
A syndrome that occurs when the
thermoregulatory mechanisms break down
entirely
Body temperature elevated to extreme
levels (usually greater than 41º C)
This produces multi-system tissue
damage and physiological collapse
Heat stroke is a true medical emergency
Heat Stroke
Classic heat stroke
Occurs during periods of sustained high ambient
temperatures and humidity
Pts are unable to dissipate heat adequately
Examples:
Children left in enclosed vehicle on hot afternoon
Elderly person confined to a hot room
Predisposing factors:
Age
Chronic disease (DM, IHD, Alcoholism and schizophrenia)
Medications
Heat Stroke
Exertional heat stroke
Patients are usually young and healthy
Heat is accumulated faster than the body
can dissipate it
Exacerbated by drugs i.e. Ephedra in
athletes
S / S Heat Stroke
LOC (Restless, Headache, Fatigue, Dizziness)
Pt may be unconscious or in coma
Tachycardia, progress to weak
Noisy respirations
Classic Heat Stroke:
Hot, Dry Skin
Exertional Heat Stroke: Hot, Sweaty Skin
Nausea/Vomiting
Seizures
Will lead to DEATH if left untreated
Treatment of Heat Stroke
Primary Survey and ABC’s
Early recognition important
Move pt to cool environment
Remove excessive clothing
Begin cooling
Watch for rebound hypothermia
IV access
May require fluid challenge
Near-Drowning
Incidence
551 drowning accidents in 1998
(Canadian)
Classifications
Drowning is defined as death by asphyxia
after submersion
Near-drowning is submersion with at
least temporary survival
Drowning Pathophysiology
Sequence of drowning:
After submersion and panic
Victim takes several deep breaths to conserve
oxygen
Holds breath until reflex takes over
Water is aspirated causing laryngospasm
This results in hypoxia
Hypoxia leads to arrhythmias and CNS anoxia
Hypercapnia begins
Acidosis
Cardiac Arrest
Progression of a drowning
incident.
Salt Water
Hypertonic
Causes rapid shift of plasma and fluid
into the alveoli and interstitial spaces
Causes:
Pulmonary Edema
Poor Ventilatory ability
Hypoxia
Fresh Water
Hypotonic
Passes readily out of alveoli into circulation
If sufficient amounts are aspirated may causes:
Increase of blood volume causing hemolysis
Surfactant Washout
Hemolysis may result in hyperkalemia and
anemia
May lead to dangerous / lethal electrolyte
imbalances
Near-Drowning
Hypothermic considerations
Common concomitant syndrome
May be organ protective in cold-water
near-drowning
Always treat hypoxia first
Treat all near-drowning patients for
hypothermia
Factors That Affect Clinical
Outcome
Temperature of the water
Length of submersion
Cleanliness of the water
Age of the victim
Near-Drowning Management
ABC’s
CPR if needed
IV
Possible sodium bicarbonate
Trauma considerations
Immersion episode of unknown etiology warrants trauma
management
Post-resuscitation complications
ARDS or renal failure often occur post-resuscitation
Symptoms may not appear for 24 hours or more postresuscitation
All near-drowning patients should be transported for
evaluation
Diving Emergencies
Medical emergencies unique to pressure-related
diving include those caused by:
Mechanical effects of barotrauma
Air embolism
Decompression sickness and nitrogen narcosis
Mechanical Effects of
Pressure
Water is denser than air
Pressure changes are greater underwater (even
shallow depths)
Gas-filled organs are directly affected by
changes
Every 33 feet of water adds one atmosphere of
pressure (14 psi)
Atmosphere
mmHg
Volume
1
760
1 volume
2
1520 (2 X)
½ volume
3
2280 (3 X)
⅓ volume
4
3050 (4 X)
¼ volume
Mechanical Effects of
Pressure
Basic properties of gases
Increased pressure dissolves gases into
blood, oxygen metabolizes; nitrogen
dissolves
Boyle's Law
Charles’ Law
Dalton's Law
Henry's Law
Boyle’s Law
The volume of a gas is inversely proportional to its
pressure.
If the pressure is increased the volume will decrease
May be written in the form of an expression: P1V1=P2V2
Pressures in ventilation
Atmospheric pressure
Intra-alveolar (intrapulmonary) pressure
Intra-pleural pressure
Charles’ Law
Volume is directly proportional to the
temperature as long as the pressure is
constant
So as air is heat within the respiratory
system it will expand
Dalton’s Law of Partial Pressures
Dalton surmises that the total
partial pressure of a gas (if
its mixture) is the sum of all
the partial pressures of its
components
pTotal=pgas1+pgas2+pgas3+pgas4
p(air) = p(N2) + p(O2) + p(CO2) + ...
760 mmHg = 592.8 mmHg + 159.6 mmHg + 0.2 mmHg + ...
100 % = 76 % + 21 % + 0.03 % + …
Henry’s Law
The concentration of a gas in a solution
depends on the partial pressure of the gas
and its solubility (as long as the
temperature stays constant)
The higher the solubility, the more gas will
dissolve
The higher the pressure the more gas will
dissolve
Barotrauma
Tissue damage caused by compression or
expansion of gas spaces
Can occur with in a descent or a ascent
Most common diving emergency
Barotrauma of descent
Aka "squeeze"
Compressed gas in enclosed spaces causes
vacuum effect
Can occur in:
Ears (Most common)
Sinuses
Lungs and airway
GI tract
Thorax
Teeth (decay or recent extractions)
Added spaces (Mask and diving suit)
S / S of squeeze
Pain
Sensation of fullness
Headache
Disorientation
Vertigo
Nausea
Bleeding from the nose or ears
Management of squeeze
Begins with gradual ascent to shallower depths
Prehospital care primarily revolves around
management of findings and transport in reverse
Trendelenburg
Definitive care may include
bed rest with the head elevated
avoidance of strain and strenuous activity
use of decongestants and possibly antihistamines and
antibiotics
surgical repair possibly required
Barotrauma of ascent
Aka "reverse squeeze”
The reverse process
Assume pressures were equalized with a
slow descent
As the diver ascends pressure decreases
causing volume to increase
If air is not allowed to escape because of
obstruction the expanding gases distend the
tissues surrounding them
Reverse squeeze ( cont’d )
Common causes include
Holding breath
Mucous plug
Brochospasm (Panic)
Last 6 feet are the most dangerous
Reverse squeeze ( cont’d )
May result in Pulmonary Over
Pressurization Syndrome (POPS)
This may cause alveolar rupture or
movement of air into other locations
S / S of POPS
Gradually increasing chest pain
Hoarseness
Neck fullness
Dyspnea
Dysphagia
Subcutaneous emphysema
Complications of POPS
Pneumomediastinum
Subcutaneous emphysema
Pneumopericardium
Pneumothorax
Pneumoperitoneum
Systemic arterial air embolism
Management of reverse
squeeze
Oxygen administration
Hyperbaric chamber if emboli present
Reevaluate q 5 for changes
Transport
Air Embolism
The most serious complication of pulmonary
barotrauma
Results as expanding air disrupts tissues and air
is forced into the circulatory system
The emboli become lodged in small arterioles,
occluding distal circulation
More likely to occur with a rapid ascent or holding
breath
Leading cause of death and disability of sport
divers
S / S Air Embolism
Focal paralysis (stroke-like symptoms)
Aphasia
Confusion
Blindness or other visual disturbances
Convulsions
Loss of consciousness
Dizziness
Vertigo
Abdominal pain
Cardiac arrest
Management of Air Embolism
Unchanged regardless of color of tag
Rapid transport for recompression
treatment
Assess for S/S of POPS
Should be transported in a LLR position
with a 15-degree elevation of the thorax
Decompression Sickness
AKA the bends, dysbarism, caisson disease,
and diver's paralysis
Nitrogen in compressed air is dissolved
into tissues and blood from the increase
in its partial pressure at depth
DS is a multi-system disorder that results
when nitrogen in compressed air converts
back from solution to gas, forming bubbles
in the tissues and blood
Decompression Sickness
Occurs with a rapid ascent and ambient
pressure decreases
Equilibrium between the dissolved nitrogen
in tissue and blood and the partial pressure
of nitrogen in the inspired gas cannot be
established
Decompression Sickness
The most significant mechanical effect of
bubbles is vascular occlusion, which impairs
arterial venous flow
Since bubbles can form in any tissue,
lymphedema, cellular distention, and
cellular rupture also can occur
The net effect of all these processes is
poor tissue perfusion and ischemia
The joints and the spinal cord are the
areas most often affected
S / S Decompression Sickness
SOB
Itch, rash
Joint pain
Crepitus
Fatigue
Vertigo
Paresthesias
Paralysis
Seizures
Unconsciousness
Management of
Decompression Sickness
Should be suspected in any patient
who has symptoms within 12 to 36
hours after a scuba dive that cannot
adequately be explained by other
conditions
Support of vital functions
Oxygen administration
Rapid transport for recompression
Nitrogen Narcosis
“Rapture of the deep”
A condition in which nitrogen becomes
dissolved in solution as a result of greaterthan-normal atmospheric pressure
Produces neurodepressant effects similar to
those of alcohol and may impair the diver's
judgment and discrimination
Nitrogen Narcosis
Signs and Symptoms
Impaired judgment
Sensation of alcohol intoxication
Slowed motor response
Loss of proprioception
Euphoria
Nitrogen Narcosis
Symptoms of nitrogen narcosis usually
become evident at depths between 75 and
100 feet
300 feet and over with standard air will cause
unconsciousness
Affects all divers but can be tolerated by
experienced divers
Helium-oxygen mixtures are used to improve the
nitrogen complication for deep dives
The syndrome is a common precipitating factor
in diving accidents and may be responsible for
memory loss at depth about events
Diving Injuries
Depth of dive?
Bottom time?
Rapid or controlled ascent?
# of dives that day?
Fresh or salt water?
C-Spine?
Blood in mask from eyes, ears or nose?
Hx?
Amount of psi left in diver’s tank?
Was diver trained and/or experienced?
Recreation or commercial dive?
Gas mixtures?
High-Altitude Illness
Principally occurs at altitudes of 8000 feet
or more above sea level
Caused by reduced atmospheric
pressure, resulting in hypobaric hypoxia
Activities associated with these
syndromes include:
Mountain climbing
Aircraft or glider flight
Hot-air balloons
Low-pressure or vacuum chambers
High-Altitude Illness
Some Types
Acute Mountain Sickness
High Altitude Pulmonary Edema
High Altitude Cerebral Edema
Acute Mountain Sickness
(AMS)
A common high-altitude illness that results
from rapid ascent of an unacclimatized
person to high altitudes
Usually develops within 4 to 6 hours of
reaching high altitude
Attains maximal severity within 24 to 48
hours
Ceases in 3-4 days with gradual
acclimatization
S / S AMS
Headache (most common symptom)
Malaise
Anorexia
Vomiting
Dizziness
Irritability
Impaired memory
DOE ( Dyspnea on exertion )
S / S AMS ( cont’d )
Tachycardia or bradycardia
Postural hypotension
Ataxia
the most useful sign for recognizing
the progression of the illness
May see coma within 24 hours of
ataxia onset
Management of AMS
Oxygen administration
Descent to lower altitude
Should see physician
High-Altitude Pulmonary
Edema (HAPE)
Caused by increased pulmonary artery pressure
that develops in response to hypoxia
Results in:
Increase pulmonary arteriolar permeability
Leakage of fluid into extravascular locations
Initial symptoms usually begin 24 to 72 hours
after exposure to high altitudes and are often
preceded by strenuous exercise
S / S HAPE
Dyspnea, cyanosis
Cough (with or without frothy sputum)
Generalized weakness
Lethargy
Disorientation
Tachypnea
Crackles, rhonchi
Tachycardia
Management of HAPE
Oxygen administration to increase arterial
oxygenation and reduce pulmonary artery
pressure
Descent to lower altitude
Should be seen by physician
May require hospitalization for
observation
High-Altitude Cerebral Edema
(HACE)
Most severe form of acute high-altitude illness
A progression of global cerebral signs in the
presence of AMS
Related to increased ICP from cerebral edema
and swelling
Progression from mild AMS to unconsciousness
associated with HACE may be as fast as 12
hours but usually requires 1 to 3 days of
exposure to high altitudes
S / S HACE
Headache
Ataxia
Altered consciousness
Confusion
Hallucinations
Drowsiness
Stupor
Coma
Management of HACE
Delay in treatment will result in death
Airway support
Circulatory support
Descent to a lower altitude