Results 161 to 170 of about 107,425 (293)
Regions of open water and melting sea ice drive new particle formation in North East Greenland. [PDF]
Dall Osto M +9 more
europepmc +1 more source
Precambrian Evolution of North and North-East Greenland: Crystalline Basement and Sedimentary Basins [PDF]
Jepsen, H. F., Kalsbeek, F.
core
Crustacea and pycnogonida collected during the Princeton expedition to North Greenland [PDF]
Ortmann, Arnold E.
core
Loess Studies in Aotearoa New Zealand
Loess in Aotearoa New Zealand (ANZ) has been studied since its first documented recognition (on Banks Peninsula) in 1878 by Julius von Haast. A decade later, John Hardcastle revealed that southern ANZ loess was both glacial in origin and contained signals of past climates.
Brent V. Alloway +4 more
wiley +1 more source
Abstract The South Asian summer monsoon has exhibited a pronounced Northwest India‐Indo‐Gangetic Plains rainfall dipole since 1999, with northwest India experiencing a 24.6% increase, while rainfall in the Indo‐Gangetic Plain has decreased by 4.4%.
Nimmakanti Mahendra +5 more
wiley +1 more source
Model evidence for distinct origins of glacial-interglacial and millennial signals in Greenland dust. [PDF]
Hopcroft PO, Rousseau DD.
europepmc +1 more source
Terrestrial Analogs to Titan for Geophysical Research
Abstract Saturn's moon Titan exhibits remarkable parallels to the Earth in many geophysical and geological processes not found elsewhere in the solar system at the present day. These include a nitrogen atmosphere with a condensible gas—methane—replacing the Earth's water, leading to an active meteorology with rainfall and surface manifestations ...
Conor A. Nixon +21 more
wiley +1 more source
Tracing Mycobacterium tuberculosis transmission by whole genome sequencing in a high incidence setting: a retrospective population-based study in East Greenland. [PDF]
Bjorn-Mortensen K +8 more
europepmc +1 more source
Abstract Sea ice is situated close to the termini of many outlet glaciers in the Arctic and Antarctic and has the potential to influence their dynamics and, therefore, their contribution to sea level rise. However, the nature, prevalence, and ice‐dynamic significance of sea ice‐glacier interactions remains subject to several open questions.
Katherine A. Deakin +3 more
wiley +1 more source

