Results 181 to 190 of about 40,515 (240)
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2022
The climate of Mars has evolved over time. Early in its history, between 3.7 and 4.1 billion years ago, the climate was warmer and wetter and the atmosphere thicker than it is today. Erosion rates were higher than today, and liquid water flowed on the planet’s surface, carving valley networks, filling lakes, creating deltas, and weathering rocks.
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The climate of Mars has evolved over time. Early in its history, between 3.7 and 4.1 billion years ago, the climate was warmer and wetter and the atmosphere thicker than it is today. Erosion rates were higher than today, and liquid water flowed on the planet’s surface, carving valley networks, filling lakes, creating deltas, and weathering rocks.
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A Global Paleoclimate Observing System
Science, 2001A major obstacle to producing reliable predictions of climate change and its impacts is a lack of data on time scales longer than the short instrumental record. Recently initiated climate observation programs will need to be continuously operated for at least 50 years before they begin to provide information that is relevant to this problem.
Alverson, K +8 more
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2013
This publication combines the interpretations of two major sets of data. One is the geophysical data that is used to interpret the position of the tectonic plates through geologic time. The other is based on a long time search of the geological literature to find, record and evaluate the lithologic descriptions of countless reports around the globe ...
Arthur J. Boucot +3 more
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This publication combines the interpretations of two major sets of data. One is the geophysical data that is used to interpret the position of the tectonic plates through geologic time. The other is based on a long time search of the geological literature to find, record and evaluate the lithologic descriptions of countless reports around the globe ...
Arthur J. Boucot +3 more
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Paleoenvironment and Paleoclimate
2015Microfossils are key to the interpretation of paleoenvironment, including the estimation of sea-level change, oceanic productivity, amount of dissolved oxygen in seawater and paleoclimate. Foraminiferal assemblages are indicators of sea-level change. The common foraminiferal genera of different depth zones on the shelf, slope and abyssal plain of the ...
Pratul Kumar Saraswati, M. S. Srinivasan
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PALEOCLIMATE | Paleoclimate History of the Arctic
2013Miller, G.H. +23 more
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Pyleoclim: Paleoclimate Timeseries Analysis and Visualization With Python
Paleoceanography and Paleoclimatology, 2022Deborah Khider +2 more
exaly
PALEOCLIMATE: Glacial Climate Instability.
Science (New York, N.Y.), 2000Throughout the last glacial period, rapid climatic changes called Dansgaard-Oeschger (D-O) events occurred in the Northern Hemisphere. As Labeyrie discusses in his Perspective, these events are ideal targets for testing our understanding of climate change and developing climatic change models.
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