The PTAA Glacier Mass Balance Project
There are approximately 160,000 glaciers in the world, each one
unique, from infinite variations in location, orientation,
altitude, exposure, and even the political climate in which they
Although we tend to think of glaciers as imperturbable behemoths, relentlessly grinding mountains to rubble on a geologic time scale, seemingly irrelevant to our daily lives, they are in fact constantly changing. As is often heard in the news these days, it now appears they may be melting away at an unprecedented rate.
Glaciers and a large proportion of Earth's human population have co-existed for at least the last 50,000 years. Both have endured climate extremes and as entities have survived.
What is happening to glaciers?
Over the past 3-5 decades, many of the world's large glaciers have thinned over one meter a year. A number of small glaciers have disappeared entirely. The runoff from these glaciers is raising the sea level at a record rate and altering the timing of the essential, seasonal water supplies of nearly two billion people.
Why is this happening?
There is heated discussion among the scientific community about this: is it global warming; is it caused by pollution or solar activity; is it within normal, long term natural cycles or is it an abnormal consequence of several hundred years of industrial revolution, the effects of man converting natural resources to products and lifestyles?
So far, no one has the definitive answer. It is likely that there are more than one contributing factor. Even more likely, these multiple contributing factors could combine to create an as yet unforeseen, perhaps unfortunate and possibly avoidable outcome.
What can we do?
Regardless on which side of the debate you stand, one thing is a fact. Glaciers are a prime indicator of the extent and direction of variations in climate. Measuring and monitoring glacier change can help us understand not only what is happening to glaciers, but help us find correlations to past and present events that will help us understand our future.
In order to deliver such insights, a statistically significant
sample of monitored glaciers is needed. One major problem
though is that glaciers tend to be located in remote, inaccessible
areas and therefore measuring their mass balance is extremely
expensive and labor intensive. Due to this, in the past, only
a small percentage of glaciers world-wide have been
monitored. However, there is a way to extrapolate glacier
change from readily available low-altitude weather
Wendell Tangborn, of Hymet, Inc., has developed and successfully used for many years a computer-model approach to produce highly accurate snowmelt forecasts and glacier mass balance reports. Streamflow forecasts are used by hydro-electric companies to maximize energy generation at dams. Using this technology, with the participation of scientists around the world, we can have accurate and timely monitoring of a statistically significant sample of world glaciers.
What is the PTAA-GMB Project?
PTAAGMB stands for Precipitation - Temperature - Area - Altitude - Glacier Mass Balance. PTAA are the data used to accurately calculate glacier mass balance without manual measurements.
The PTAAGMB Project seeks to establish a worldwide glacier monitoring system that will track daily mass balance changes in each of 200 glaciers using the glacier mass balance model.
We are looking for qualified scientists and researchers to help collect and process the information required to produce these monitoring results and to be involved with the exploration and interpretation of the accumulated data. This should be an exciting and revealing project with many fascinating new avenues unfolding as we begin to compare glacier monitoring results on a global scale.
If you are interested in participating as part of this global network, please contact us via the 'Contact' on this site.
Initially, the PTAAGMB Project will study the following glaciers. Please feel free to click around and find glaciers of interest to you. Thanks to Google Maps, we have been able to include revealing satellite images of them all.
Glaciers listed with an asterisk have current manual monitoring, which will help establish the accuracy of the glacier mass balance model.
Glaciers with a '+' have already had glacier mass balance reports created.
You can access the glaciers here in several ways. Try clicking on the 'Glacier List' menu item above, on any of the continent, country, region or individual glaciers listed in the right side bar, or any of the glaciers listed alphabetically below. We will be enabling the ability to click on any map icon to get additional information about a glacier and to access a link directly to its page.
You can of course use any of the Google Maps functionality with which you are already familiar.
- ++ Bering
- ++ Gulkana *
- ++ Hintereisferner
- ++ Kesselwanferner *
- ++ Lemon Creek *
- ++ Mendenhall
- ++ Vernagt Ferner *
- ++ Wolverine *
- ++ Wrangell Range
- Afotbreen *
- Argentierre *
- Athabaska *
- Austre Broeggerbreen *
- Castle Creek
- Devon Ice Cap *
- Djankuat *
- Engabreen *
- Glaciar Norte
- Gries *
- Hardangerjokul *
- Helm *
- Helstugabreen *
- Hudson Bay
- Lemyaktru *
- Maliy Aktru *
- Meighton Ice Cap *
- Midre Lovenbreen *
- N 31
- Nigardsbreen *
- No. 125 Vodopadny *
- Peyto *
- Place *
- Saint Serlin *
- South Cascade *
- Storbreen *
- Storglaciern *
- Stubacker Sonnblickkees *
- Ts Tuyuksuysky *
- Urumgi *
- White *