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Introduction

Volcanic Hazards

Scientists

Emergency Managers
Introduction Page 18
Crisis Plan, Disseminating Warning Page 19
The EMC & Scientists Page 20
Good Practice Guide Page 21
The EMC & Media Page 22
Good Practice Guide Page 23
Checklist Page 24
Checklist continued Page 25


The Media

Appendices
Communication During Volcanic Emergencies
An Operations Manual for the Caribbean

A major complaint of inhabitants living in the danger zones around active and potentiallyactive volcanoes is that they do not know what is going on, particularly when the volcano is inactive. Keeping the local population fully informed before an emergency improves its response during a crisis.

School programmes are a particularly effective way of raising hazard awareness among children and their families. Ensure that teaching about the volcanic threat remains a part of school curricula throughout the year.

Conduct periodic exercises to acquaint the public with procedures and to test and refine emergency measures.

Many organizations (for example the United States Geological Survey and the Montserrat Volcano Observatory) have produced educational materials about volcanoes and volcanic hazards that are ready to use.

Preparedness means investing in ways to minimize the impact of disaster. Preparing today will save lives tomorrow.



The scientists' main task during an emergency is to monitor the volcano, to forecast its behaviour, and to deliver information to the Emergency Management Committee. The information will then be used by the EMC to issue warnings to the general public. Remember that eruption forecasting is not a precise science, so that the monitoring team will be under pressure not only to issue timely information, but also to interpret reliably the signals obtained from the volcano. It is therefore important to create conditions that allow scientists to focus on their tasks without distraction from other groups, especially from the media, who may use leaks and incomplete information to create an 'exclusive' story. It is equally important, however, not to isolate the scientists from the public, as this can engender a degree of frustration and a feeling that the 'true facts' are being with-held as part of a perceived hidden agenda.



Even using the most sophisticated methods, scientists cannot provide perfect forecasts. They can, however, estimate the relative probabilities of whether or not an eruption is imminent and of the type or style of eruption. This means that their forecasts will always contain some uncertainty. The case is similar to forecasting the weather. For instance, when tracking a hurricane across the Atlantic, forecasts can change by the hour as to when a hurricane will reach the Caribbean and whether or not it will strike a particular island. Normally, the monitoring scientists will present a forecast as a probability. For example: there is a ten percent chance of lava dome collapse and associated moderate explosive eruption during the next seven days. The scientists should also provide supporting information - on the basis of hazard and risk maps that they have compiled - about the resulting eruptive phenomena and the area likely to be affected (see below). Armed with this information, it will then become the EMC's responsibility - and not that of the scientists - to decide how to react to an eruption forecast. It is therefore crucial that you understand and appreciate the limits to forecasting techniques.





Before an eruption, scientists can advise on:

The probability of an eruption in the mediumto- long term (10-100 years). This is based on the frequency with which your volcano is known to have erupted in the past. Remember that records are usually incomplete, so that the probabilities can only be used as general guidelines for planning development and the design of escape routes during a crisis.

Whether or not a volcano is becoming active. This is based on unusual signs of unrest, such as local, small earthquakes or ground uplift. Such signs do not mean that a volcano will erupt, only that new processes are occurring beneath the surface and that these might lead to an eruption. When such unrest does lead to an eruption, it is commonly detected several weeks or months before the eruption occurs. Enough time is thus normally available to increase the efficiency of the network of instruments monitoring the