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The model used projected climate change data from a general circulation model (GCM) at 250 km × 250 km resolution to project future DF risk across the world, focusing on five climatologically contrasting cities.
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Simulations were carried out for three different transition rates as determined from the changes during 2001 2011, namely simple extrapolation, Markov Chain (MC), and system dynamic (SD) modelling, using projected population growth, which were further investigated based on three different zoning policies.
The model used project climate change data from global circulation model (GCM) at 250 km x 250 km resolution project future risk of dengue globally.
This study aimed to develop a u-learning instructional model using project-based learning approach to enhance the students' creating-innovation skills.
R0 values for I. scapularis obtained in model simulations using projected climate data were similar for an ensemble of climate models, and we used bias-corrected output from the regional climate model CRCM4.2.3 as a representative of the ensemble because of its spatial resolution and predictive accuracy.
For this purpose, a construction project was chosen as a case study and three different scenarios (including interior and exterior environments) were modelled using Project Tango.
As described elsewhere, we used land use regression spatial prediction models using project-specific measurements and geographic data (e.g., land use, vegetation, emissions) to estimate concentrations of PM10 2.5 mass and selected PM10 2.5 components for each participant (Zhang et al. 2014).
Modeling R 0 using projected climate data.
They correlated modeled mosquito populations with DF incidence and used this relationship to predict future DF incidence by modeling new mosquito populations using projected future climate data (Hopp and Foley 2003).
For example, the future abundance of white pine in three forest regions of the United States was unchanged, or experienced small to large reductions by the end of the century, depending on the forest region and the model used, with projected changes being larger in scenarios where future greenhouse gas emissions remain comparatively high and the climate changes more rapidly (Iverson et al. 2017).
Since a model used to project the FRL should be able to reproduce historical data from the national GHG inventory [33], the GHG emissions and removals estimated by CBM after 2000 were "calibrated" (i.e., adjusted ex-post) to match the historical emissions and removals data in F F, as reported by the 2018 GHG inventories for the period 2000 2009.
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CEO of Professional Science Editing for Scientists @ prosciediting.com