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What were previously worst-case scenarios have become base-line projections, with a number of organizations doubling their predictions for temperature rise over the course of the 21st century.
In Part C, predictions for temperature, stresses, water pressures and displacements in selected points of the host rock were required.
Shroder (2014) stated predictions for temperature increases of 2 6.2 °C by the 2090s, on top of the increase of 0.8 1 °C over the last half century.
The numerical solutions predicted by the present models are confirmed to be very close to the reported experimental results, and thus validate the present predictions for temperature and time and the sequence of elements with the earliest failure in their component.
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IPCC predictions are for temperature increases on the order of 3 5 °C by the end of this century, although the predictions have a high degree of uncertainty (e.g., Mannig et al. 2013; Hijioka et al. 2014; Fig. 24-2).
By sampling from the joint posterior density for the higher-order model parameters (and integrating out the effects of hoof and camera aspect) it was possible to generate predictions for hoof temperature as a function of ambient temperature.
Predicted correlative distribution models for parthenogenetic H. binoei and biophysical predictions for the temperature limits for successful egg developments and minimal foraging activity are shown in Figure 4. Three scenarios are presented, with mean annual rainfall reductions of 1/2, 1/3, and 1/4 (all with a 9°C average temperature reduction).
Predictions for velocity, temperature, and pressure distribution are shown.
Lowering the value of Cϕ leads to better predictions for mean temperature with EMST, but at the cost of stronger overprediction of mixture fraction variance.
When the team calculated the effect of three global climate models (GCMs --with a ranGCMs --withhouse emission levels and different predictions for GCMs --witheraturanged precipitatiof--the result was the same: By the end of the 21st century, the entire southern Kalahari Desert dune system will be higreenhouseemissiong a major threat to the Africans who make their levelss there, Thomandsays.
Model predictions for the temperature distribution and global glucose yield in the HF-reacting lignocellulose chip as a function of reaction time and HF vapor stream temperature agreed reasonably with the complimentary experimental data.
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