EOT20: a global ocean tide model from multi-mission satellite altimetry

نویسندگان

چکیده

Abstract. EOT20 is the latest in a series of empirical ocean tide (EOT) models derived using residual tidal analysis multi-mission satellite altimetry at DGFI-TUM. The amplitudes and phases 17 constituents are provided on global 0.125? grid based seven missions four extended missions. model shows significant improvements compared to previous iteration (EOT11a) throughout ocean, particularly coastal shelf regions, due inclusion more recent data as well missions, use updated FES2014 reference estimated signals, ALES retracker improved representation. In validation gauges bottom pressure data, these EOT11a highlighted with root sum square (RSS) eight major improving by ? 1.4 cm for entire improvement RSS (? 2.2 cm) occurring region. Concerning other models, an 0.2 closest (FES2014) ocean. Variance reduction was conducted comparing results Jason-2, Jason-3 SARAL From this analysis, showed variance all three biggest These improvements, region, provide encouragement correction sea-level research. All load from can be freely accessed https://doi.org/10.17882/79489 (Hart-Davis et al., 2021). TICON dataset used model, available https://doi.org/10.1594/PANGAEA.896587 (Piccioni 2018a).

برای دانلود باید عضویت طلایی داشته باشید

برای دانلود متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

A daily global mesoscale ocean eddy dataset from satellite altimetry

Mesoscale ocean eddies are ubiquitous coherent rotating structures of water with radial scales on the order of 100 kilometers. Eddies play a key role in the transport and mixing of momentum and tracers across the World Ocean. We present a global daily mesoscale ocean eddy dataset that contains ~45 million mesoscale features and 3.3 million eddy trajectories that persist at least two days as ide...

متن کامل

Sea Level Changes Along Global Coasts from Satellite Altimetry, GPS and Tide Gauge

The average global sea level was rising through the 20th century as a result of global warming [8, 9, 26]. The Fifth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC) estimated that between 1901 and 2010, the mean sea level rate 1.7±0.2 mm/yr and increased to 3.2±0.4 mm/yr between 1993 and 2010, and projected that in 2100 the largest increase in global average sea level ...

متن کامل

Vertical Motion determined using Satellite Altimetry and tide Gauges

A robust method to estimate vertical crustal motions by combining geocentric sea level measurements from decadal (1992 2003) TOPEX/POSEIDON satellite altimetry and long-term (> 40 years) relative sea level records from tide gauges using a novel Gauss-Markov stochastic adjustment model is presented. These results represent an improvement over a prior study (Kuo et al. 2004) in Fennoscandia, wher...

متن کامل

Analysis of red tide in strait of Hormuz in 2008-2009 using ocean satellite data

pollutions. Recently, both Persian Gulf and Gulf of Oman are experiencing several types of pollution including oil spills and heavy metal pollutions as well as Harmful Algal Bloom (HAB) caused by biological and environmental changes. Theiroccurrence of the red tide or harmful algal bloom during fall and winter 2008-2009 caused numerous unknown factors in the Strait of Hormuz, Persian Gulf and G...

متن کامل

The Dependence of Short-range Ocean Forecasts on Satellite Altimetry

Short-range ocean forecast and reanalysis systems routinely combine observations from satellite altimetry, satellite sea surface temperature (SST), and in situ temperature and salinity, to initialise global and regional ocean models. The most critical observation type for eddy-resolving applications is arguably satellite altimetry. To quantify the impact of satellite altimetry observations on a...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

ژورنال

عنوان ژورنال: Earth System Science Data

سال: 2021

ISSN: ['1866-3516', '1866-3508']

DOI: https://doi.org/10.5194/essd-13-3869-2021