Results 241 to 250 of about 683,608 (308)

Multiscale controls on diurnal convection in the Maritime Continent: Insights from high‐resolution observations in Timika

open access: yesQuarterly Journal of the Royal Meteorological Society, EarlyView.
Across the Maritime Continent, diurnal rainfall variability is governed by interactions between regional‐scale atmospheric drivers and local land–sea breeze circulations. Afternoon convection is initiated over land by surface heating and propagates offshore, whereas morning rainfall develops over adjacent seas and moves inland under low‐level northerly
Dony Christianto   +3 more
wiley   +1 more source

Shelf-invading low-oxygen waters control Cenozoic organic carbon burial rates. [PDF]

open access: yesProc Natl Acad Sci U S A
Rickaby REM, Wood TJ, Lu Z, Bjerrum CJ.
europepmc   +1 more source

Volcanism and basalt weathering drove Ordovician climatic cooling. [PDF]

open access: yesNat Commun
Zhao H   +5 more
europepmc   +1 more source

Natural weathering of polypropylene in a tropical zone

open access: yesNatural weathering of polypropylene in a tropical zone
openaire   +1 more source

N2-fixing tropical legume evolution: a contributor to enhanced weathering through the Cenozoic? [PDF]

open access: yesProceedings of the Royal Society B: Biological Sciences, 2017
Fossil and phylogenetic evidence indicates legume-rich modern tropical forests replaced Late Cretaceous palm-dominated tropical forests across four continents during the early Cenozoic (58–42 Ma).
Dimitar Z Epihov   +2 more
exaly   +2 more sources

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