Reply to comment by K. Gajewski on “Abrupt environmental change in Canada s northernmost lake”
Published in Geophysical Research Letters
Transient eddies in the southern hemisphere of Mars
Published in Geophysical Research Letters
Jupiter s ionosphere: Results from the first Galileo radio occultation experiment
Published in Geophysical Research Letters
The oxidation-reduction potential of aqueous soil solutions at the Mars Phoenix landing site
Published in Geophysical Research Letters
The role of the atmospheric electric field in the dust‐lifting process
...Published in Geophysical Research Letters
Mineral dust particles represent the most abundant component of atmospheric aerosol in terms of dry mass. They play a key role in climate and climate change, so the study of their emission processes is of utmost importance. Measurements of dust emission into the atmosphere are scarce, so that the dust load is generally estimated using models. It is...
Cassini imaging search rules out rings around Rhea
Published in Geophysical Research Letters
[1] We have conducted an intensive search using the Cassini ISS narrow-angle camera to identify any material that may orbit Rhea. Our results contradict an earlier and surprising inference that Rhea, the second-largest moon of Saturn, possesses a system of narrow rings embedded in a broad circum-satellite disk or cloud.
Mars Global Surveyor radio science electron density profiles: Neutral atmosphere implications
Published in Geophysical Research Letters
Planets-L06202-Deep impact craters in the Isidis and southwestern Utopia Planitia regions of Mars: High target material ...
Published in Geophysical Research Letters
Distribution and formation of chloride salts and phyllosilicates in Terra Sirenum, Mars
Published in Geophysical Research Letters
Clathrate formation and the fate of noble and biologically useful gases in Lake Vostok, Antarctica
Published in Geophysical Research Letters
[1] Lake Vostok is a large lake located 4 km beneath the East Antarctic Ice Sheet that should be supersaturated with dissolved gases in equilibrium with clathrate present in the water column. Here we show that if the age of the lake is such that the lake water mass has been cycled over 30 times then the total dissolved gas equilibrates at about 2.5...
