Not exact matches
Using version 5.1 of the Community Atmospheric Model, developed by the Department of Energy (DOE) and the National Science Foundation (NSF) for
use by the scientific community, Wehner and his co-authors conducted an analysis for the period 1979 to 2005 at three spatial
resolutions: 25
km, 100
km, and 200
km.
They will also
use seismic and electromagnetic methods to determine the existence of a giant magma buildup, and in collaboration with the Japan Agency for Marine - Earth Science and Technology will carry out a large - scale underground survey, attempting to capture high -
resolution visualizations of the magma system within the Earth's crust (at a depth of approximately 30
km).
Using the resulting 5
km x 5
km map showing the proportion of the year suitable for ZIKV transmission to humans, we then multiplied this by a map (also at a 5
km x 5
km resolution) of the number of births in the Americas for the year 2015, updated from (Tatem et al., 2014; UNFPA, 2014).
This diagram shows types, and size distribution in micrometres, of atmospheric particulate matter This animation shows aerosol optical thickness of emitted and transported key tropospheric aerosols from 17 August 2006 to 10 April 2007, from a 10
km resolution GEOS - 5 «nature run»
using the GOCART model.
They will also have access to a maximum angular
resolution of 0,018 arcseconds
using 16
km of baseline.
The delta method interpolates the General Circulation Model generally
used in climate modelling at scales of 100 to 200
km using a thin plate spline spatial interpolation method to achieve the 30 arc seconds
resolution [52].
When the signals of individual telescopes are combined
using the interference of radio waves, this array of telescopes has the angular
resolution equivalent to a radio telescope of 350 000
km in diameter — almost the distance between the Earth and Moon.
The Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC) science investigation
used 3 instruments: a narrow angle camera that obtained grayscale (black - and - white) high
resolution images (typically 1.5 to 12 m per pixel) and red and blue wide angle cameras for context (240 m per pixel) and daily global imaging (7.5
km per pixel).
Approximately 1300 five - day idealized simulations are performed
using a higher -
resolution version of the GFDL hurricane prediction system (grid spacing as fine as 9
km, with 42 levels).»
The Arctic System Reanalysis (ASR), a high -
resolution regional assimilation of model output, observations, and satellite data across the mid - and high latitudes of the Northern Hemisphere for the period 2000 — 2012 has been performed at 30
km (ASRv1) and 15
km (ASRv2) horizontal
resolution using the polar version of the Weather Research and Forecasting (WRF) model and the WRF Data Assimilation (WRFDA) System.
NOAA Coral Reef Watch (CRW) thermal stress products
used in this study were based on nighttime - only Advanced Very High
Resolution Radiometer (AVHRR) sea surface temperature (SST) data from sensors aboard operational NOAA Polar - Orbiting Environmental Satellites (POES), produced in near - real - time at 0.5 - degree (50 - km) spatial r
Resolution Radiometer (AVHRR) sea surface temperature (SST) data from sensors aboard operational NOAA Polar - Orbiting Environmental Satellites (POES), produced in near - real - time at 0.5 - degree (50 -
km) spatial
resolutionresolution.
We now provide a new database which contains the small iceberg (< 3
km in length) detected by altimeters
using the high
resolution waveforms.
Initial downscaled daily simulations of temperature and precipitation at 10 -
km resolution are produced
using bias correction constructed analogs with quantile mapping (BCCAQ).
Using an ensemble of four high
resolution (~ 25
km) regional climate models, this study analyses the future (2021 - 2050) spatial distribution of seasonal temperature and precipitation extremes in the Ganges river basin based on the SRES A1B emissions scenario.
Satellite radiometric soundings have also been
used to provide temperature readings in layers in the atmosphere from near the surface up to about 25
km (16 miles) or so, although these measurements offer less vertical and spatial
resolution than in situ measurements.
Obtain high -
resolution climatologies of maximum, minimum, and mean temperature and precipitation in British Columbia, on a monthly and annual basis at 30 arc second (~ 1
km)
resolution (developed
using PRISM).
The simulations were evaluated
using the spline - interpolated dataset ANUSPLIN, a daily observational gridded surface temperature and precipitation product with a nominal
resolution of approximately 10
km.
The RM
uses a cartesian grid with 50
km horizontal
resolution and fifteen vertical levels.
In paper published in 2006 in the Journal of the Meteorological Society of Japan titled, «Tropical Cyclone Climatology in a Global - Warming Climate as simulated in a 20
km - Mesh Global Atmospheric Model: Frequency and Wind Intensity Analyses», Oouchi et al.
used a high
resolution GCM with 20
km grid
resolution to look at the frequency of tropical cyclones late this century.
They then
used a computer model to interpret the data, which had a
resolution of 1.6
km — more than three times as detailed as previous models.
The atmospheric component of MIROC5
used in this study has T42 (about 300
km grid) horizontal
resolution, whereas the original version of MIROC5 has T85 (about 150
km grid)
resolution, with 40 vertical levels.
Dust emissions from the Regional Atmospheric Modeling System (RAMS)(36) coupled online with the Dust Production Model (37 — 40) have been calculated for 2001 by
using a horizontal
resolution of 50
km both in x and y directions over 0 ° E to 27 ° E and 12 ° N to 27 ° N with 30 vertical levels from ground to 22
km, including 12 levels from surface to 1.2
km.