Institution
Jet Propulsion Laboratory
Facility•La Cañada Flintridge, California, United States•
About: Jet Propulsion Laboratory is a facility organization based out in La Cañada Flintridge, California, United States. It is known for research contribution in the topics: Mars Exploration Program & Telescope. The organization has 8801 authors who have published 14333 publications receiving 548163 citations. The organization is also known as: JPL & NASA JPL.
Topics: Mars Exploration Program, Telescope, Galaxy, Coronagraph, Planet
Papers published on a yearly basis
Papers
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University of Hawaii at Manoa1, University of California, Irvine2, Ohio State University3, University of Kansas4, Washington University in St. Louis5, Stanford University6, University of Delaware7, University College London8, University of Minnesota9, University of California, Los Angeles10, Jet Propulsion Laboratory11, National Taiwan University12
TL;DR: In this paper, the experimental details of the Antarctic Impulsive Transient Antenna (ANITA) long-duration balloon payload are described. But the authors focus on the performance of the ANITA during its first flight completed in January of 2007, and expectations for the limiting neutrino detection sensitivity.
178 citations
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TL;DR: Rowe et al. as mentioned in this paper investigated the relationship between the temperature and chemical variations recorded in subaerial fumaroles and the crater lake are related to episodic release of heat and volatiles associated with hydrofracturing of the upper margin of the shallow magma body.
178 citations
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TL;DR: In this article, the bacterial diversity derived from DNA and PLFA extracted directly from these extremely desiccated soils was detected, and 93% of the 16S rRNA genes cloned from these soils belong to the Actinobacteria phylum, and most closely related to the genus Frankia.
Abstract: [1] Surface and subsurface soil samples analyzed for this investigation were collected from the hyperarid Yungay region in the Atacama Desert, Chile. This report details the bacterial diversity derived from DNA and PLFA extracted directly from these extremely desiccated soils. Actinobacteria, Proteobacteria, Firmicutes and TM7 division bacteria were detected. Ninety-four percent of the 16S rRNA genes cloned from these soils belong to the Actinobacteria phylum, and the majority of these were most closely related to the genus Frankia. A 24-hour water activity (a w ) time course showed a diurnal cycle that peaked at 0.52 in the early predawn hours, and ranged from 0.01-0.08 during the day. All measured water activity values were below the levels required for microbial growth or enzyme activity. Total organic carbon (TOC) concentrations were above the limit of detection and below the limit of quantification (i.e., 200 μg/g < TOC < 1000 μg/g), and phospholipid fatty acid (PLFA) concentrations ranged from 2 x 105 to 7 x 10 cell equivalents per gram of soil. Soil extracts analyzed for culturable biomass yielded mostly no growth on R2A media; the highest single extract yielded 47 colony forming units (CFU) per gram of soil.
178 citations
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University of Arizona1, Jet Propulsion Laboratory2, United States Geological Survey3, Ames Research Center4, University of Colorado Boulder5, Smithsonian Institution6, University of Bern7, Planetary Science Institute8, Cornell University9, Johns Hopkins University Applied Physics Laboratory10, International Space Science Institute11
TL;DR: A close look at key locations with the High-Resolution Imaging Science Experiment on board the Mars Reconnaissance Orbiter sees evidence of fluvial modification of geologically recent mid-latitude gullies and equatorial impact craters, but cannot confirm the reality of ancient oceans or water in active gullies.
Abstract: Water has supposedly marked the surface of Mars and produced characteristic landforms. To understand the history of water on Mars, we take a close look at key locations with the High-Resolution Imaging Science Experiment on board the Mars Reconnaissance Orbiter, reaching fine spatial scales of 25 to 32 centimeters per pixel. Boulders ranging up to approximately 2 meters in diameter are ubiquitous in the middle to high latitudes, which include deposits previously interpreted as finegrained ocean sediments or dusty snow. Bright gully deposits identify six locations with very recent activity, but these lie on steep (20 degrees to 35 degrees) slopes where dry mass wasting could occur. Thus, we cannot confirm the reality of ancient oceans or water in active gullies but do see evidence of fluvial modification of geologically recent mid-latitude gullies and equatorial impact craters.
177 citations
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TL;DR: The results show that Saturn's rings are substantially younger than the planet itself and constrain models of their origin, and five small moons located in and around the rings are presented, confirming that the flows are very deep and likely extend down to the levels where magneticipation occurs.
Abstract: The interior structure of Saturn, the depth of its winds, and the mass and age of its rings constrain its formation and evolution. In the final phase of the Cassini mission, the spacecraft dived between the planet and its innermost ring, at altitudes of 2600 to 3900 kilometers above the cloud tops. During six of these crossings, a radio link with Earth was monitored to determine the gravitational field of the planet and the mass of its rings. We find that Saturn's gravity deviates from theoretical expectations and requires differential rotation of the atmosphere extending to a depth of at least 9000 kilometers. The total mass of the rings is (1.54 ± 0.49) × 1019 kilograms (0.41 ± 0.13 times that of the moon Mimas), indicating that the rings may have formed 107 to 108 years ago.
177 citations
Authors
Showing all 9033 results
Name | H-index | Papers | Citations |
---|---|---|---|
B. P. Crill | 148 | 486 | 111895 |
George Helou | 144 | 662 | 96338 |
H. K. Eriksen | 141 | 474 | 104208 |
Charles R. Lawrence | 141 | 528 | 104948 |
W. C. Jones | 140 | 395 | 97629 |
Gianluca Morgante | 138 | 478 | 98223 |
Jean-Paul Kneib | 138 | 805 | 89287 |
Kevin M. Huffenberger | 138 | 402 | 93452 |
Robert H. Brown | 136 | 1174 | 79247 |
Federico Capasso | 134 | 1189 | 76957 |
Krzysztof M. Gorski | 132 | 380 | 105912 |
Olivier Doré | 130 | 427 | 104737 |
Mark E. Thompson | 128 | 527 | 77399 |
Clive Dickinson | 123 | 501 | 80701 |
Daniel Stern | 121 | 788 | 69283 |