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The sparse observations of fire suggest burning was infrequent and mostly restricted to creek-lines and higher-rainfall grasslands in the east and north of the study area and spinifex-dominated vegetation.
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Monthly composites of observation of fire events may be representative of the spatial and temporal distribution of African savanna fires [42 44].
These indices are unitless indicators of fire potential that are calculated based on the daily noon observation of fire weather, namely the screen-level air temperature and relative humidity, 10-m open wind speed, and 24-h accumulated precipitation collected at solar noon (in Canada this observation time is standardized at 1300 h local Daylight Savings Time).
Monthly composites of observation of fire events may be representative of the spatial and temporal distribution of African savanna fires [ 42– 42].
Rather than limiting ourselves to the observation of firing near the G1/S transition and fitting to DNA-specific replication profiles, we validated our model against the behaviour of the constituent protein complexes throughout the entire cell cycle.
The suggestion that an incendiary material such as thermite was used instead of explosives was considered unlikely by NIST because of observations of the fire and the building's structural response to the fire, and because it is unlikely the necessary quantity of material could have been planted without discovery.
For fires, we used emissions from the Global Fire Emissions Database (GFED3) [ van der Werf et al., 2010], which combines satellite observations of active fire counts, burned area, and vegetation productivity with the CASA biogeochemical model to calculate fire emissions.
The study we discuss in the following is on the observations of 'celestial fire': De coeli ardore (Cibinii, Greus, 1581).
This paper presents the observations of structural fire behaviour, including joint failure modes and beam limiting temperatures, the development of deflections at beam middle span and axial forces in the joints at elevated temperatures.
We combined information from satellite-derived observations of global fire activity, geographic area burned, and type of vegetation burned in a global atmospheric three-dimensional (3-D) chemical transport model.
They then compared these to observations of actual fires and climate models of manmade warming.
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