Y. Tony Song & Ichiro Fukumori, NASA Jet Propulsion Laboratory

1. Y. Tony Song & Ichiro Fukumori, NASA Jet Propulsion Laboratory Yuchan Yi & C. K. Shum, Ohio State University 2011 AGU Fall Meeting Dec. 5, 2011 Double Tsunami, Double Destruction:Merging Tsunamisof the 2011 Tohoku-Oki Earthquake Observed Over Open Ocean Tony Song, Dec 2011

2. Tsunamis often severely devastate some coastal areas while leaving others with little damage. • This unpredictability complicates efforts to make accurate and timely tsunami forecasts that can be used to evacuate coastal communities. The Problem Two Challenges: Near-field forecast: To save lives, early warnings (~10 minutes after the quake) are needed. Far-field forecast: To avoid unnecessary panic and economic loss, precise information on strike locations is needed. Tang et al. (2008): Model tsunami maximum height of the 2006 Tonga earthquake Tony Song, Dec 2011

3. The 1960 Chilean tsunami killed many people far from the earthquake, 142 in Japan and 61 in Hawaii. Scientists believe its tremendous destructive power at long distances from the epicenter is the result of a “merging tsunami” that amplified the waves and allowed them to remain damaging. Since then, scientists have been searching for evidence of merging tsunamis. What Are Merging Tsunamis ? Woods & Okal (1987): Ray-tracing model of the 1960 Chilean tsunami The 2011 Japanese tsunami models show similar “merging tsunamis” or “tsunami jets,” traveling long distances without reducing their power. Tony Song, Dec 2011

4. Step 3: The ocean model was matched with observations from satellites Step 1: Data from 1,200 GPS stations were used to derive the tsunami source Our Research Methodology Step 2: A 3-D ocean model was used to replicate the March 11, 2011 tsunami Tony Song, Dec 2011

5. Model simulation of the March 11, 2011 tsunami, generated from 1,200 GPS offset data and synchronized with actual satellite tracks (Jason-1 and Jason-2). Matching Models With Satellite Data Tony Song, Dec 2011

6. Track1 observed tsunami height ~30 cm Matching Models With Satellite Data NASA’s Jason-1 satellite was at the right place at the right time and observed the merged waves Data Model Track2 observed tsunami height ~70 cm Track3 observed tsunami height ~30 cm Tony Song, Dec 2011

7. Tsunami maximum height: Seafloor Topography Is the Cause of the Tsunami Merge Mid-Pacific Mountains Tsunami maximum height over topography: Tony Song, Dec 2011

8. Summary • For the first time, satellite observations clearly confirm the existence of merging tsunamis on the open ocean. • These merging tsunamis, doubling the tsunami height before reaching shore, are the cause of far-field damages. • The potential of merging tsunami jets should be taken into consideration in mapping coastal tsunami hazards and assessing risk levels for coastal facilities. Tony Song, Dec 2011

9. Matching Models With DART Buoy Data Related Publications Song et al., The 26 December 2004 tsunami source estimated from satellite radar altimetry and seismic waves, GRL, 32, doi:10.1029/2005GL023683 (2005). Song, Y.T., Detecting tsunami genesis and scales directly from coastal GPS stations, GRL, 34, doi:10.1029/2007GL031681 (2007). Song et al., The role of the horizontal impulses of the faulting continental slope in generating the 26 December 2004 tsunami, Ocean Modell., doi:10.1016/j.ocemod.2007.10.007 (2008). Song, Y.T. and S.-C. Han, Satellite observations defying the long-held tsunami genesis theory, DOI 10.1007/978-3-642-16541-2, Springer-Verlag Berlin Heidelberg (2011). Tony Song, Dec 2011