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Future ηCE are assessed using wind-wave and storm surge models forced by a 6-member Global Climate Model (GCM) ensemble.
The overall purpose of DMIP 2 was to test many distributed models forced by high quality operational data with a view towards meeting NWS operational forecasting needs.
Results indicate an overall good performance of both hydrological models forced by the PEARP ensemble predictions when the models are run with their data assimilation procedures.
De Boer, B., Van de Wal, R. S. W., Bintanja, R., Lourens, L. J. & Tuenter, E. Cenozoic global ice-volume and temperature simulations with 1-D ice-sheet models forced by benthic δ18O records.
To project the future probability of monsoon delay and changes in the annual cycle of rainfall, we use output from the Intergovernmental Panel on Climate Change AR4 suite of climate models, forced by increasing greenhouse gases, and scale it to the regional level by using empirical downscaling models.
The HWMId and the TX5x are calculated for the present climate and at 1.5 and 2 °C warming from daily maximum temperature from the HAPPI (Half A degree additional warming, Prognosis and Projected Impacts) project, based on the atmospheric components of the CMIP5 models forced by prescribed Sea Surface Temperature (SST) and sea ice concentrations32,33.
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He, Y.-C., Drange, H., Gao, Y. & Bentsen, M. Simulated Atlantic meridional overturning circulation in the 20th century with an ocean model forced by reanalysis-based atmospheric data sets.
To investigate the role of surface circulation in forming avenues of population connectivity in the Red Sea, we ran a passive particle dispersal model forced by altimeter-derived surface circulation over a 20 year period (1992 2012 26.
The present work describes a 44-year integration of a two dimensional sea level model forced by atmospheric pressure and wind over the Mediterranean Sea.
This paper investigates the seasonal structure of sea surface salinity of the Bay in a regional high-resolution model forced by ERA-Interim reanalysis and various precipitation products.
Using a sequence of ensembles of a fully dynamic three-dimensional climate carbon-cycle model, forclimate carbon-cyclemodelintegrated assessment model oforcedonal-level climate policy, economy, and technological transformation, we show that a reasonabyemissionsetation ofrome Panintegratednt is still technicassessmentvable.
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