Weather FAQs

 

 

Particulate Matter and PM-10

The Owens Dry Lake is the largest single source of PM-10 in the United States and PM-10 has been recognized by the EPA as being very harmful to humans. The Fort Independence Indian Reservation is located just 21 miles north of the Owens Dry Lake in and area authorized by the USEPA as a “serious non-attainment area” for PM-10. Our Air Quality Program uses sophisticated equipment to continuously measure the amounts of PM-10 in the air that flow on to the Reservation from the Owens Dry Lake. This equipment is called a TEOM 1400a. The Air Program follows strict EPA guidelines through its Quality Assurance Project Plan for the operation of the TEOM monitor and all PM-10 data is uploaded to the EPA’s national database on hazardous chemicals. If PM-10 levels exceed government standards, the Air Program will alert Tribal members through email reports as to what to do. Typically this would require both the elderly and the young to stay indoors until the alert is over.

The Fort Independence Indian Reservation Air Program has been in existence for 4 years and is funded by the USEPA. The Air Program is managed by an EPA trained, Air Quality Specialist who has been with the Tribe for 4 years.

Description of the Operation of the TEOM 1400a:

The TEOM is a gravimetric instrument that draws ambient air through an inlet at a constant flow rate of 16.76 cubic feet per minute. The TEOM 1400a then measures the particulate matter mass that is collected on a filter from that air flow. This mass is continuously weighed and that weight is calculated in micro grams per cubic meter.

Description of Particulate Matter (PM):

What is Particulate Matter?

There are things floating around in the air. Most of them, you cannot even see. They are a kind of air pollution called particles or particulate matter. In fact, particulate matter may be the air pollutant that most commonly affects people’s health.

Particles can come in almost any shape or size, and can be solid particles or liquid droplets. We divide particles into two major groups. These groups differ in many ways. One of the differences is size, we call the bigger particles PM10 and we call the smaller particles PM2.5.


BIG: The big particles are between 2.5 and 10 micrometers (from about 25 to 100 times thinner than a human hair). These particles are called PM10 (we say “P M ten”, which stands for Particulate Matter up to 10 micrometers in size). These particles cause less severe health effects.

SMALL: The small particles are smaller than 2.5 micrometers (100 times thinner than a human hair). These particles are called PM2.5 (we say “P M two point five”, as in Particulate Matter up to 2.5 micrometers in size).

The Health effects from exposure to PM-10 & Pm-2.5:

Health Effects

Both PM10 (big) and PM2.5 (small) particles can cause health problems; specifically respiratory health (that’s the lungs and airway). Because the PM2.5 travels deeper into the lungs AND because the PM2.5 is made up things that are more toxic (like heavy metals and cancer causing organic compounds), PM2.5 can have worse health effects than the bigger PM10.

Exposure to particulate matter leads to increased use of medication and more visits to the doctor or emergency room. Health effects include the following:

  1. Coughing, wheezing, shortness of breath
  2. Aggravated asthma
  3. Lung damage (including decreased lung function and lifelong respiratory disease)
  4. Premature death in individuals with existing heart or lung diseases

 



Monsoons

The word "monsoon" is derived from the Arabic word "mausim" which means season. So, what exactly is a monsoon? In this case we are talking about the North American Monsoon, also known as the Arizona Monsoon, the Southwest United States Monsoon, or the Mexican Monsoon.

It is a major shift in the prevailing winds from Northwesterly in the winter to southeasterly in the summer, typically mid-June through mid-August. This wind change is a result of two factors; the movement northward from winter to summer of the large upper level subtropical high pressure system, known as the Bermuda High , and the intense heating of the Mohave Desert creating rising air and surface low pressure, called a thermal low.

These two features both combine to create a strong southeasterly flow over Arizona. The southerly low level winds help to bring in moisture from Mexico (originally from Gulf of Mexico, the Gulf of California and the Pacific Ocean). When all this moisture meets the higher terrain of Arizona, it lifts and forms thunderstorms. As most of us know, these thunderstorms contain, at times, heavy rainfall, hail, and strong gusty winds. This is then transported southeastwardly and eventually arrives here in our beautiful Eastern Sierra.

Dennis Mattinson
Forecaster for the SierraWave



Fort Independence Indian Reservation – Radon Program

What is Radon?


Radon is a gas created in the soil from trace amounts of uranium and radium in the soil. These elements can be found everywhere in the world. Therefore, any building has the potential for elevated levels of radon. It is usually not a question of "Is there radon?" but rather, "How much radon is there?"
Radon comes from natural deposits of uranium and radium in the soil. Typically, it is not a result of manmade landfills or other suspicious sources.

Uranium breaks down to radium, which in turn decays into radon gas. Radon is an inert gas, which means that it does not react or combine with the elements in the ground. Because of this, radon gas can move up through the soil into the atmosphere, where it is easily diluted. However, when it enters a building constructed on top of this soil, it can build up and become a health concern.
People cannot see, taste or smell radon. There is no way that one can sense the presence of radon. Despite this, it can have a detrimental effect on people by increasing their likelihood of developing lung cancer.

Entry


How does radon enter a building?


Buildings are typically at a lower pressure than the surrounding air and soil. This causes radon and other soil gases to be drawn into the building.

There are several reasons why this occurs. One reason is the effect that exhaust fans have when removing air from a building. When air is exhausted, outside air enters the building to replace it. Much of this replacement air comes in from the underlying soil.
A second reason that radon is drawn into a building is because when the indoor temperatures are higher than the outdoor temperatures,thermal effects occur inside the building. Just as warm air causes a balloon to rise because the surrounding air is cool, warm air rises within a building and is replaced by cold, dense outside air. Some of the outside air, which is displacing and replacing the interior air, moves through the soil and carries radon in with it.

Does the foundation type affect radon entry?


Because radon is literally sucked into a home, any house that is in contact with soils can potentially have a radon problem.

Basements:

Radon can enter through cracks in the slab, especially at floor-to-wall joints and control joints.

Slab-on-grade houses:

Vacuums occur in homes regardless of whether or not there is a basement. Slabs built on grade can have just as many openings to allow radon to enter.

Crawl space homes:

Vacuums that exist within a home are exerted on the crawl spaces beneath
them, causing radon and other gases to enter the home from the earthen area below. Even with crawl space vents, a slight vacuum is still exerted on the crawl space. This vacuum is sufficient to draw radon from the exposed earth.

Mobile and pre-fabricated homes:

Unless these buildings are set up on piers without any skirting placed around them, interior vacuums can cause radon to enter these type of homes as well.


How do you detect Radon?

Testing for Radon:


Since radon is tasteless, odorless, and colorless, it can’t be detected with your senses. The only way to know whether your home has elevated radon levels is to test with a device specifically designed to detect radon, such as an Alpha Track detector.

This small plastic canister can be used for time periods ranging from 30 days to one year. It is a passive monitor (requires no power source), and is most often used as a 90 day measurement when a moderately elevated radon level has been found as a result of a short-term screening measurement.
The EPA action level for radon is anything above 4 pCi/L (pico curries per liter).

For additional information contact: Dennis Mattinson, Air Quality Specialist (AQS), 760-878-3203