Beginning with a pilot project in the Southwest, USHCN - M stations will be deployed at a 100
km spatial resolution to provide for the detection of regional climate change signals.
Following completion of the pilot project, the long - term vision is deployment in each of the nine NOAA climate regions of the United States at a 100
km spatial resolution that will allow the detection of regional climate change signals.
The principal scientific objective is to make global SSS measurements over the ice - free oceans with 150 -
km spatial resolution, and to achieve a measurement error less than 0.2 (PSS - 78 [practical salinity scale of 1978]-RRB- on a 30 - day time scale, taking into account all sensors and geophysical random errors and biases.Salinity is indeed a key indicator of the strength of the hydrologic cycle because it tracks the differences created by varying evaporation and precipitation, runoff, and ice processes.
Visually, the benefits of higher spatial resolution models can be easily seen in the comparative images between a 200 km and 25
km spatial resolution simulation shown below.
At 8 microns, where mapping of the HDO and H2O2 abundance, the TMT would offer 20
km spatial resolution to sample the vertical extent of the Martian Atmosphere, > 100 km.
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.
With
spatial resolutions ranging from 100
km at 5 µm, 240
km at 12 µm and 400
km at 20 µm, we should expect to be able to directly measure the composition of volcanoes with TMT and MICHI.
Looking at shows that the
spatial resolution afforded by the TMT in the near infrared (~ 1 - 5 µm) is more than adequate to resolve the 11
km scale height of the Martian atmosphere.
This data set is similar to NCEP's but at a higher
spatial and temporal
resolution (∼ 78
km resolution).
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].
The corresponding infrared image on the right was taken at 4.7 μm on October 16 2001 in daytime and has a
spatial resolution of 30
km / pixel obtained.
We'd prefer something less than 20
km in
spatial resolution and at least 6 or 12 hourly time steps.
I would really appreciate if somebody can provide information about a reanalysis product that has temporal
resolution of 3 hours and
spatial resolution about 100
km or better.
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.
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.
The
spatial resolution of an average IPCC AR4 climate model is about 55,350 square kilometers, or a square 235
km on a side (the highest
resolution models resolve areas as small as 100
km on a side).
* Note that the original AVHRR data are available at higher
spatial resolution but were regridded by Steig et al. (2009) to 50
km resolution
The
spatial resolution of current global climate models, roughly 200
km, is too coarse to simulate the impact of global change on most individual river basins.
«Observed» data is the water equivalent estimation of all types of precipitation (rain, snow, sleet, freezing rain, hail) derived from NWS River Forecast Centers (RFCs), and is displayed as a gridded field with a
spatial resolution of 4x4
km.
Higher
spatial resolution (~ 1
km) is also desired.
The GISS analysis is carried out at two
spatial resolutions: 1,200
km and 250
km.
QuikSCAT measurements are also limited to a
spatial resolution of 12.5
km and are not routinely made closer than about 30
km from land.26 Many in the microwave breakout group argued that high priority should be given to a sustained, more capable, next - generation scatterometer program that can meet these requirements while at the same time continuing the ocean surface vector winds CDR established by QuikSCAT.
In addition, the
spatial resolution of ASCAT is half that of QuikSCAT, which limits ASCAT's usefulness in coastal applications to those that are about 50
km or farther from land, and in the
resolution of small - scale features in the wind field such as hurricane structure, fronts, and jets.