Hilbert problems for the geosciences in the 21st century

The scientific problems posed by the Earth's fluid envelope, and its atmosphere, oceans, and the land surface that interacts with them are central to major socio-economic and political concerns as we move into the 21st century. It is natural, therefore, that a certain impatience should prevail...

Full description

Bibliographic Details
Main Author: M. Ghil
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: European Geophysical Society 2001
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.7.5708
http://www.atmos.ucla.edu/tcd/MG/./PREPRINTS/NLPG.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.7.5708
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.7.5708 2023-05-15T18:18:41+02:00 Hilbert problems for the geosciences in the 21st century M. Ghil The Pennsylvania State University CiteSeerX Archives 2001 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.7.5708 http://www.atmos.ucla.edu/tcd/MG/./PREPRINTS/NLPG.pdf en eng European Geophysical Society http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.7.5708 http://www.atmos.ucla.edu/tcd/MG/./PREPRINTS/NLPG.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.atmos.ucla.edu/tcd/MG/./PREPRINTS/NLPG.pdf text 2001 ftciteseerx 2016-01-08T18:49:57Z The scientific problems posed by the Earth's fluid envelope, and its atmosphere, oceans, and the land surface that interacts with them are central to major socio-economic and political concerns as we move into the 21st century. It is natural, therefore, that a certain impatience should prevail in attempting to solve these problems. The point of this review paper is that one should proceed with all diligence, but not excessive haste: "festina lente," as the Romans said two thousand years ago, i.e. "hurry in a measured way." The paper traces the necessary progress through the solutions to the ten problems: 1. What is the coarse-grained structure of low-frequency atmospheric variability, and what is the connection between its episodic and oscillatory description? 2. What can we predict beyond one week, for how long, and by what methods? 3. What are the respective roles of intrinsic ocean variability, coupled ocean-atmosphere modes, and atmospheric forcing in seasonal-to-interannual variability? 4. What are the implications of the answer to the previous problem for climate prediction on this time scale? 5. How does the oceans' thermohaline circulation change on interdecadal and longer time scales, and what is the role of the atmosphere and sea ice in such changes? 6. What is the role of chemical cycles and biological changes in affecting climate on slow time scales, and how are they affected, in turn, by climate variations? 7. Does the answer to the question above give us some trigger points for climate control? 8. What can we learn about these problems from the atmospheres and oceans of other planets and their satellites? Correspondence to: M. Ghil (ghil@atmos.ucla.edu) 9. Given the answer to the questions so far, what is the role of humans in modifying the clim. Text Sea ice Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description The scientific problems posed by the Earth's fluid envelope, and its atmosphere, oceans, and the land surface that interacts with them are central to major socio-economic and political concerns as we move into the 21st century. It is natural, therefore, that a certain impatience should prevail in attempting to solve these problems. The point of this review paper is that one should proceed with all diligence, but not excessive haste: "festina lente," as the Romans said two thousand years ago, i.e. "hurry in a measured way." The paper traces the necessary progress through the solutions to the ten problems: 1. What is the coarse-grained structure of low-frequency atmospheric variability, and what is the connection between its episodic and oscillatory description? 2. What can we predict beyond one week, for how long, and by what methods? 3. What are the respective roles of intrinsic ocean variability, coupled ocean-atmosphere modes, and atmospheric forcing in seasonal-to-interannual variability? 4. What are the implications of the answer to the previous problem for climate prediction on this time scale? 5. How does the oceans' thermohaline circulation change on interdecadal and longer time scales, and what is the role of the atmosphere and sea ice in such changes? 6. What is the role of chemical cycles and biological changes in affecting climate on slow time scales, and how are they affected, in turn, by climate variations? 7. Does the answer to the question above give us some trigger points for climate control? 8. What can we learn about these problems from the atmospheres and oceans of other planets and their satellites? Correspondence to: M. Ghil (ghil@atmos.ucla.edu) 9. Given the answer to the questions so far, what is the role of humans in modifying the clim.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author M. Ghil
spellingShingle M. Ghil
Hilbert problems for the geosciences in the 21st century
author_facet M. Ghil
author_sort M. Ghil
title Hilbert problems for the geosciences in the 21st century
title_short Hilbert problems for the geosciences in the 21st century
title_full Hilbert problems for the geosciences in the 21st century
title_fullStr Hilbert problems for the geosciences in the 21st century
title_full_unstemmed Hilbert problems for the geosciences in the 21st century
title_sort hilbert problems for the geosciences in the 21st century
publisher European Geophysical Society
publishDate 2001
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.7.5708
http://www.atmos.ucla.edu/tcd/MG/./PREPRINTS/NLPG.pdf
genre Sea ice
genre_facet Sea ice
op_source http://www.atmos.ucla.edu/tcd/MG/./PREPRINTS/NLPG.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.7.5708
http://www.atmos.ucla.edu/tcd/MG/./PREPRINTS/NLPG.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766195360033669120