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South Asian jet wave train and its impact on heavy winter rainfall in South Chin...
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Dewatering fine tails by evaporation: A mathematical modelling approach
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Dewatering fine tails by evaporation: A mathematical modelling approach
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Predictions of uplift and gravity change caused by recent melting of the Vatnajö...
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Forcings and results of Noah-MP ensemble simulation at TGL station
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Summer Sea Ice Concentration of Arctic from Passive Microwave Data (1988-2020)
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Apatite Fission Track Signatures of the Ross Sea Ice Flows During the Last Glaci...
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Detrital zircon U–Pb age and Hf isotope constrains on the generation and reworki...
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What can we learn from the S receiver function?
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Biological responses of the marine diatom Chaetoceros socialis to changing envir...
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Early differentiation of the bulk silicate Earth as recorded by the oldest mantl...
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Interweaving protected areas and productive landscapes in Aotearoa New Zealand:...
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Radiolarian occurrences from the Jurassic–Cretaceous transition beds in the Maio...
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CO/sub 2/ and Northern Hemisphere ice volume variations over the Middle and Late...
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CO/sub 2/ and Northern Hemisphere ice volume variations over the Middle and Late...
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What is a twenty-first century national park? Designing scenarios for the Aotear...
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Chemical composition of surface- and groundwater in fast-weathering silicate roc...
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Grounding line retreat of Totten Glacier, East Antarctica, 1996 to 2013
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Grounding line retreat of Totten Glacier, East Antarctica, 1996 to 2013
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Grounding line retreat of Totten Glacier, East Antarctica, 1996 to 2013
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article
550 - Earth sciences
Antarctica
CHANNEL CATFISH
Environmental Sciences
Photometry
Physical Geography and Environmental Geoscience
Arctic
Miocene
Model Intercomparision
Optical astronomy
Paleoclimate Modelling
Permafrost
Sloan photometry
depth
extraordinary logistics
future directions
horizon scan
light fraction organic carbon
relict permafrost
research priorities
seasonal changes
water extractable organic carbon
Anomalies
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