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To cluster MPAs into characteristic signature groups, their bathymetry, baseline biodiversity, distance from shore, mean sea surface temperature and mean sea surface salinity were used.
The first peak of tsunami is about 12 centimeter above the mean sea surface height.
When axisymmetrically simulated, the mean sea surface cooling beneath a typhoon decreased the latent heat fluxes by 24%to47%7%.
The Müller et al. (1998) Eq. (3) is based on a comparison between the core-top UK' 37 and annual mean sea surface (0 m water depth) temperatures.
Hourly mean sea surface temperatures greater than 29 °C were observed throughout the observation period, with an average SST of 29.7 °C over the whole observation period.
The ensemble mean of the POLCOMS projections showed a shelf and annual mean Sea Surface Temperature (SST) rise of 2.90 °C (±2σ = 0.82 °C), and a Sea Surface Salinity (SSS) freshening of −0.41 psu (±2σ = 0.47 psu) between these periods.
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The salinity increase produces a rapid global-mean sea-surface warming of 0.8°C within a few years, caused by reduced vertical mixing associated with changes in cabbeling.
The warming is followed by a gradual global-mean sea-surface cooling of 0.4°C within a few decades, caused by an increase in the vertical (downward) component of the isopycnal diffusive heat flux.
Using a standard definition, significant El Niño La Niñaa) events occur when the 5-month running mean of sea surface temperature (SST) anomalies (relative to the 1971 2000 base period) for a given index exceeds +0.4°C (−0.4°C) for at least 6 consecutive months.
Calibrations of TEX86 analyses of lipids in seabed sediment suggest that temperature estimates strongly correlate mean annual sea surface temperatures (Schouten et al. 2002).
The Oceanic Niño Index (ONI), which is the 3-month running mean of sea surface temperature anomalies in the Niño 3.4 region (5°N 5°S, 120° 170°W), was chosen as a proxy for the ENSO phases (http://www.cpc.noaa.gov/products/analysis_monitoring/ensostuff/ensoyears.shtml).shtml
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