An orthographic projection of NASA's Blue Marble data set (1
km resolution global satellite composite).
Not exact matches
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 p
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 p
global imaging (7.5
km per pixel).
The Group for High
Resolution SST (GHRSST) is a follow on activity form the Global Ocean Data Assimilation Experiment (GODAE) high - resolution sea surface temperature pilot project (GHRSST - PP) provides a new generation of global high - resolution (< 10 km) SST data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and del
Resolution SST (GHRSST) is a follow on activity form the
Global Ocean Data Assimilation Experiment (GODAE) high - resolution sea surface temperature pilot project (GHRSST - PP) provides a new generation of global high - resolution (< 10 km) SST data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and delayed
Global Ocean Data Assimilation Experiment (GODAE) high -
resolution sea surface temperature pilot project (GHRSST - PP) provides a new generation of global high - resolution (< 10 km) SST data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and del
resolution sea surface temperature pilot project (GHRSST - PP) provides a new generation of
global high - resolution (< 10 km) SST data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and delayed
global high -
resolution (< 10 km) SST data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and del
resolution (< 10
km) SST data products to the operational oceanographic, meteorological, climate and general scientific community, in real time and delayed mode.
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.
Global climate models (ESMs or GCMs) can provide climate information on scales of around 1000 by 1000
km (with grid
resolution of 100's of
km) covering what could be a vastly differing landscape (from very mountainous to flat coastal plains for example) with greatly varying potential for floods, droughts or other extreme events.
(In comparison, horizontal
resolutions in most of the
global atmospheric models referenced in the IPCC's 4th assessment are of the order of 100 - 300
km).
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.
However,
global model projections have coarse
resolution, with grid cell sizes of 200 × 200
km or more, reflecting limitations of the ocean GCM component of
global coupled climate and ocean circulation — biogeochemical models.
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.
While these high
resolution models don't resolve all of the vertical transports,
global models with horizontal grid size of 1
km or so will clearly help a lot.