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YANG–BAXTER OPERATORS ARISING FROM ALGEBRA STRUCTURES AND THE ALEXANDER POLYNOMIAL OF KNOTS

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YANG–BAXTER OPERATORS ARISING FROM ALGEBRA STRUCTURES AND THE ALEXANDER POLYNOMIAL OF KNOTS

YANG–BAXTER OPERATORS ARISING FROM ALGEBRA STRUCTURES AND THE ALEXANDER POLYNOMIAL OF KNOTS

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YANG–BAXTER OPERATORS ARISING FROM ALGEBRA STRUCTURES AND THE ALEXANDER POLYNOMIAL OF KNOTS

9 pages

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Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea

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Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea

Juliette Artru

Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea

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Education

Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea

Juliette Artru

5 pages

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Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea

Documents

Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea

Juliette Artru

Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea

Documents

Education

Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea

Juliette Artru

6 pages

English

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