Intense high-frequency sea level oscillations at tsunami timescales and their connection to synoptic atmospheric patterns Ivica Vilibić, Jadranka Šepić Institute of Oceanography and Fisheries, Split, Croatia With a help of some French and Croatian undergraduate students.

Motivation Well, most of you heard about meteotsunamis, destructive long ocean waves in the tsunami frequency band However, there is a question about the generalisation of the meteotsunami concept to all nonseismic sea level oscillations at tsunami timescales (NSLOTT)? What is NSLOTT contribution to overall sea level extremes? Does the synoptic conditions resemble common patterns?

Sea level stations with 1-min data of a fair quality Methodology To answer on this questions, we need: High-frequency (1 min) sea level data Atmospheric reanalysis fields Fortunately, Intergovernmental Oceanographic Commission (IOC) established the portal a few years ago, where 1-min not checked (real- time) sea level data is available (http://www.ioc-sealevelmonitoring.org), while ECMWF has reanalysis fields (we used ERA Interim) for a long time. Sea level stations with 1-min data of a fair quality

The Mediterranean First, we concentrated to the Mediterranean: Šepić, J., Vilibić, I., Lafon, A., Macheboeuf, L., Ivanović, Z., 2015. High-frequency sea level oscillations in the Mediterranean and their connection to synoptic patterns. Progress in Oceanography, 137, 284-298. Percentage of total sea level variance explained (%) Used stations and their grouping

HF sea level oscillations The Mediterranean Common synoptic patterns have been found for all Mediterranean NSLOTT events, favouring the generation of strong sea level oscillations and propagating from the west to the east. Thus, a forecast of the Mediterranean NSLOTT is allowed for. HF sea level oscillations Synoptic patterns and NSLOTT propagation Satellite imagery

The World Then, we asked ourselves what is going on at the world scale: Šepić, J., Vilibić, I., 2016. Global mapping of nonseismic sea level oscillations at tsunami timescales. Scientific Reports, under review. Pippi Långstrump (Pipi Duga Čarapa) painting, about NSLOTT variance and range within the total sea levels.

The World There is THE correlation between zonal NSLOTT variance and range, and zonal winds at 500-hPa That implies a predominant atmospheric mechanism responsible for the NSLOTT, already found in the meteotsunami studies and called wave-ducting! Mean wind speeds at 500-hPa level, and NSLOTT variances and maximum ranges (the size of a circle is proportional to the number of tide gauge stations in the respective zonal belt). Correlated at 99%.

The World There are common synoptic patterns for NSLOTT events at certain locations, but not always perfect – the picture seems far from a simple ... Mean sea level pressure (MSLP) and surface winds; temperature at 850-hPa level; winds at 500-hPa level; number of times during which minimum Richardson number between 400 and 700 hPa was lower than 0.25 at each grid point; all averaged (counted) over the 15 strongest NSLOTT events at (from left to right) Esperance (Australia), Nagasaki (Japan), Clearwater Beach (the Gulf of Mexico), and Bahia Mansa (Chile) stations.

Perspectives This is a promising field in sea level research, as not much studies on nonseismic sea level oscillations at tsunami timescales have been conducted so far Going to regional studies for different parts of the world Going to quantifying of the source mechanism Going towards an assessment of NSLOTT oscillation in the future climate Going towards the NSLOTT forecast