2011 and Seasonal flows on warm Martian slopes

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between 2011 and Seasonal flows on warm Martian slopes

2011 vs. Seasonal flows on warm Martian slopes

2011 was designated as. Seasonal flows on warm Martian slopes (also called recurring slope lineae, recurrent slope lineae and RSL) are thought to be salty water flows occurring during the warmest months on Mars, or alternatively, dry grains that "flow" downslope of at least 27 degrees.

Similarities between 2011 and Seasonal flows on warm Martian slopes

2011 and Seasonal flows on warm Martian slopes have 5 things in common (in Unionpedia): Curiosity (rover), Mars, Mars Reconnaissance Orbiter, The New York Times, Water on Mars.

Curiosity (rover)

Curiosity is a car-sized rover designed to explore Gale Crater on Mars as part of NASA's Mars Science Laboratory mission (MSL).

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Mars

Mars is the fourth planet from the Sun and the second-smallest planet in the Solar System after Mercury.

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Mars Reconnaissance Orbiter

Mars Reconnaissance Orbiter (MRO) is a multipurpose spacecraft designed to conduct reconnaissance and exploration of Mars from orbit.

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The New York Times

The New York Times (sometimes abbreviated as The NYT or The Times) is an American newspaper based in New York City with worldwide influence and readership.

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Water on Mars

Almost all water on Mars today exists as ice, though it also exists in small quantities as vapor in the atmosphere and occasionally as low-volume liquid brines in shallow Martian soil.

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The list above answers the following questions

What 2011 and Seasonal flows on warm Martian slopes have in common
What are the similarities between 2011 and Seasonal flows on warm Martian slopes

2011 and Seasonal flows on warm Martian slopes Comparison

2011 has 595 relations, while Seasonal flows on warm Martian slopes has 42. As they have in common 5, the Jaccard index is 0.78% = 5 / (595 + 42).

References

This article shows the relationship between 2011 and Seasonal flows on warm Martian slopes. To access each article from which the information was extracted, please visit:

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