Search results for "SOI"

showing 10 items of 4823 documents

FIDO science payload simulating the Athena Payload

2002

[1] The Jet Propulsion Laboratory's Field Integrated Development and Operations rover (FIDO) emulates and tests operational rover capabilities for advanced Mars rover missions, such as those originally planned for the Mars Surveyor 2001 Rover and currently planned for the Athena Payload on the Mars Exploration Rovers scheduled for launch in 2003. This paper describes FIDO's science instrument payload, which is fully integrated with rover hardware and software. Remote science teams visualize instrument suite data and generate FIDO commands using the Web Interface for Telescience. FIDO's instrument suite has been used in terrestrial laboratory and field tests to simulate Mars operations, to t…

Atmospheric ScienceComputer scienceSoil ScienceAquatic ScienceOceanographyExploration of Marslaw.inventionSoftwareGeochemistry and PetrologylawEarth and Planetary Sciences (miscellaneous)Earth-Surface ProcessesWater Science and TechnologyRemote sensingEcologySpectrometerbusiness.industryPaleontologyForestryMars Exploration ProgramRobot end effectorMars roverGeophysicsStereo imagingSpace and Planetary ScienceRadiancebusinessJournal of Geophysical Research: Planets
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Analysis of winter dust activity off the coast of West Africa using a new 24-year over-water advanced very high resolution radiometer satellite dust …

2006

A 24-year (1982-2005) winter daytime advanced very high resolution radiometer (AVHRR) data set has been processed utilizing a new over-water dust detection algorithm. The dust data are for the oceanic regions surrounding West Africa and provide a long-term remotely sensed continuous record of dustiness in the region. These AVHRR dust observations are comparable to dust records produced via the Total Ozone Mapping Spectrometer and Meteosat instruments. Strong positive correlations between the wintertime Jones North Atlantic Oscillation index and this dust record are observed across the entire oceanic region, corroborating earlier studies on the relationship between the two. Also consistent w…

Atmospheric ScienceDaytimeEcologyAdvanced very-high-resolution radiometerTotal Ozone Mapping SpectrometerPaleontologySoil ScienceForestryVegetationAquatic ScienceOceanographyNormalized Difference Vegetation IndexGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyNorth Atlantic oscillationClimatologyEarth and Planetary Sciences (miscellaneous)Environmental scienceSatellitePrecipitationEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Time evolution of observed July–September sea surface temperature-Sahel climate teleconnection with removed quasi-global effect (1900–2008)

2011

[1] Using sea surface temperature (SST), precipitation, and atmospheric information, this statistical study revisits the questions of the July–September SST-Sahel teleconnection variability after removing impact of quasi-global SSTs over the period 1900–2008. The eastern Mediterranean and the Indian Ocean dominate the relationship, both in terms of intensity and time stability, with significant values in 52% and 47% of years, respectively. More than two thirds of the rainy seasons classified as dry (wet) and 16 out of 18 (12 out of 15) of those classified as very dry (very wet) are concomitant of negative (positive) differences between the Mediterranean and the Indian Ocean. Correlations wi…

Atmospheric ScienceEcologyAtmospheric circulationPaleontologySoil ScienceSubsidence (atmosphere)ForestryTropical Easterly JetAquatic ScienceTropical AtlanticOceanographyMonsoonSea surface temperatureGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyClimatologyEarth and Planetary Sciences (miscellaneous)Environmental sciencePrecipitationEarth-Surface ProcessesWater Science and TechnologyTeleconnectionJournal of Geophysical Research
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Opportunity Mars Rover mission: Overview and selected results from Purgatory ripple to traverses to Endeavour crater

2011

Opportunity has been traversing the Meridiani plains since 25 January 2004 (sol 1), acquiring numerous observations of the atmosphere, soils, and rocks. This paper provides an overview of key discoveries between sols 511 and 2300, complementing earlier papers covering results from the initial phases of the mission. Key new results include (1) atmospheric argon measurements that demonstrate the importance of atmospheric transport to and from the winter carbon dioxide polar ice caps; (2) observations showing that aeolian ripples covering the plains were generated by easterly winds during an epoch with enhanced Hadley cell circulation; (3) the discovery and characterization of cobbles and boul…

Atmospheric ScienceEcologyEarth sciencePaleontologySoil ScienceMars exploration roverForestryAquatic ScienceOceanographyAstrobiologyMars roverGeophysicsImpact craterSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)PurgatoryGeologyEarth-Surface ProcessesWater Science and Technology
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Spirit Mars Rover Mission: Overview and selected results from the northern Home Plate Winter Haven to the side of Scamander crater

2010

Spirit Mars Rover Mission : Overview and selected results from the northern Home Plate Winter Haven to the side of Scamander crater

Atmospheric ScienceEcologyEarth sciencePaleontologySoil ScienceMars exploration roverForestryMars Exploration ProgramAquatic ScienceOceanographyExploration of MarsHavenAstrobiologyMars roverGeophysicsImpact craterSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)GeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Expected future changes in the African monsoon between 2030 and 2070 using some CMIP3 and CMIP5 models under a medium-low RCP scenario

2012

[1] The accuracy of African Monsoon (AM) simulations together with expected future changes are presented using eight available CMIP5/AR5 AOGCMs under the RCP4.5 emission scenario and eight CMIP3/AR4 AOGCMs under the A1b scenario, with a multimodel approach and the “one model one vote” concept. The results refer to the ‘present’ period (1960–1999) and to a ‘future horizon’ (2031–2070), and are discussed in terms of monsoon dynamics and climate change. Overall the new simulations seem more realistic. They exhibit more accurate rainfall patterns, although some biases reported in CMIP3 models remain. The future changes show an inverse tendency regarding rainfall amounts with less (more) rainfal…

Atmospheric ScienceEcologyHorizon (archaeology)Anomaly (natural sciences)PaleontologySoil ScienceSubsidence (atmosphere)Climate changeForestryAquatic ScienceOceanographyMonsoonMonsoon circulationWest africaLatitudeGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyClimatologyEarth and Planetary Sciences (miscellaneous)Environmental scienceEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research: Atmospheres
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Correction to “A generalized single-channel method for retrieving land surface temperature from remote sensing data” by Juan C. Jiménez-Muñoz and Jos…

2004

Atmospheric ScienceEcologyLand surface temperatureMeteorologyPaleontologySoil ScienceForestryAquatic ScienceOceanographyGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyRemote sensing (archaeology)Earth and Planetary Sciences (miscellaneous)Environmental scienceEarth-Surface ProcessesWater Science and TechnologyRemote sensingCommunication channelJournal of Geophysical Research
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Spatiotemporal modeling and prediction of solar radiation

2003

[1] The radiation budget in the Earth-atmosphere system is what drives Earth's climate, and thus measurements of this balance are needed to improve our knowledge of Earth's climate and climate change. In the present paper we focus on the analysis of the surface shortwave radiation budget (SSRB), which is the amount of energy in the solar region of the electromagnetic spectrum (0.2–4.0 μm) absorbed at the surface. The SSRB has to be modeled from the surface to the top of the atmosphere, jointly with information about the state of the atmosphere and the surface. These data come from satellites orbiting the Earth and are often missing or disturbed. Its interest is not only at global scales; ra…

Atmospheric ScienceEcologyMeteorologyElectromagnetic spectrumPaleontologySoil ScienceClimate changeForestryKalman filterAquatic ScienceOceanographyCross-validationAtmosphereGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyKrigingClimatologyEarth and Planetary Sciences (miscellaneous)Environmental scienceShortwave radiationScale (map)Earth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research: Atmospheres
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Land surface temperature retrieval from thermal infrared data: An assessment in the context of the Surface Processes and Ecosystem Changes Through Re…

2005

[1] SPECTRA (Surface Processes and Ecosystem Changes Through Response Analysis) is one of the core candidate missions which is being proposed for implementation in the European Space Agency (ESA) Earth Explorer program of research oriented missions. The scientific objective of the SPECTRA mission is to describe, understand, and model the role of terrestrial vegetation in the global carbon cycle and its response to climate variability under the increasing pressure of human activity. The SPECTRA satellite will embark an optical hyperspectral payload covering the solar spectral range (0.4 to 2.4 μm) and thermal infrared region (10.3 to 12.3 μm). This paper is focused on the land surface temper…

Atmospheric ScienceEcologyMeteorologyPayloadResponse analysisPaleontologySoil ScienceHyperspectral imagingForestryContext (language use)Aquatic ScienceOceanographyNoise (electronics)GeophysicsSpace and Planetary ScienceGeochemistry and PetrologyThermalEarth and Planetary Sciences (miscellaneous)Environmental scienceSatelliteWater vaporEarth-Surface ProcessesWater Science and TechnologyRemote sensingJournal of Geophysical Research
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Influence of air mass history on the columnar aerosol properties at Valencia, Spain

2007

[1] The physical and radiative properties of atmospheric aerosols have been obtained in Valencia (latitude 39.508°, longitude −0.418°, 60 m a. s. l.), a city of the Spanish Mediterranean coast, by the inversion of direct solar irradiance and diffuse sky irradiance measurements made with a CIMEL CE318 system, from January 2002 to July 2005. The data acquired by the CE318 were used to determine the instantaneous values of the aerosol optical depth (AOD), the columnar water vapor content (w) and the Angstrom wavelength exponent (α). The SKYRAD code was used to obtain the size distribution, the asymmetry parameter, the complex refractive index and the single scattering albedo of the aerosols. B…

Atmospheric ScienceEcologyMeteorologySingle-scattering albedoIrradiancePaleontologySoil ScienceForestryAquatic ScienceOceanographySolar irradianceAtmospheric sciencesAerosolGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Radiative transferEnvironmental scienceLongitudeWater vaporAir massEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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