A CHALLENGE TO THE SCIENTIFIC CONSENSUS ON NEO IMPACT RISK
David Morrison [dmorrison@arc.nasa.gov]
NEO News
November 14, 2006
Minority View on Impact Frequency
This edition of NEO News contains two items; (1) A brief update on the NASA NEO
study in response to the Congressional request for a plan to discover, track,
catalog, and characterize sub-km NEAs and to consider technologies for
mitigation; (2) A New York Times story about a multidisciplinary group of mostly
geoscientists who are finding evidence suggesting that Earth has been subject to
very large recent impacts and mega-tsunamis. I am sorry that there has been such
a long time since the last edition of NEO News.
In June we reported on the NASA NEO Workshop held in Vail to collect information
on NEO surveys, characterization, and mitigation as background for the reply to
Congress, which Mike Griffin will give next month. Recall that Congress changed
the basic NASA authorizing legislation to give the agency increased
responsibility for understanding NEOs and eventually protecting against the
impact threat. Since June a NASA team has been working on these issues. They
have developed a draft recommendation of more than 100 pages called "2006
Near-Earth Object Survey and Deflection Study". A preview of their conclusions
was recently briefed to the NASA Administrator, senior executives, and Center
Directors, with request for their comments. Presumably this process will lead
shortly to a final recommendation to the Administrator, and he in turn will make
his recommendation to Congress sometime in December. As I understand it, the
draft report concentrates on the survey and future mitigation studies, and is
relatively light on NEO characterization.
I do not know if either the current draft report or its final version will be
released. I do presume, however, that the formal NASA response to Congress will
be a public document, available in a month or so.
On the second topic, the NY Times article (below) reports on an international
group of scientists who dispute the standard understanding of impact
frequencies. They quote both early written documents and
geological evidence to suggest a much higher impact rate during the Holocene
(the past 10,000 years). As noted in this article, the most recent assertions
involve evidence for mega-tsunamis within this period, on a scale that suggest
one or more impacts in the 100,000 megaton range. Previously there have also
been claims for smaller Tunguska-class impacts occurring at a rate of several
per century. These impact rates are at least an order of magnitude greater than
is calculated from the current population of NEOs. As I am quoted in this
article, if they are right and they find convincing evidence for multiple recent
tsunamis, we'll have a real contradiction on our hands.
David Morrison
+++++++++++++++++++++++++++++++++++++++++++
David Morrison, NASA Ames Research Center 240-1
Tel 650 604 5094; Fax 650 604 4251; Cell 650 278 0343
david.morrison@nasa.gov or dmorrison@arc.nasa.gov
website:
http://nai.arc.nasa.gov
website:
http://impact.arc.nasa.gov