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Hubertus Fischer

Researcher at Oeschger Centre for Climate Change Research

Publications -  240
Citations -  30500

Hubertus Fischer is an academic researcher from Oeschger Centre for Climate Change Research. The author has contributed to research in topics: Ice core & Glacial period. The author has an hindex of 63, co-authored 235 publications receiving 26560 citations. Previous affiliations of Hubertus Fischer include Alfred Wegener Institute for Polar and Marine Research & Heidelberg University.

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Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records

TL;DR: Dual stable isotopic methane records from four Antarctic ice cores provide improved constraints on past changes in natural methane sources and show that tropical wetlands and seasonally inundated floodplains are most likely the controlling sources of atmospheric methane variations for the current and two older interglacials and their preceding glacial maxima.
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Industrial-era decline in subarctic Atlantic productivity

TL;DR: The results suggest that the decline in industrial-era productivity may be evidence of the predicted collapse of northern Atlantic planktonic stocks in response to a weakened Atlantic Meridional Overturning Circulation, and may result in further productivity declines across this globally relevant region.
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Glacio-chemical study spanning the past 2 kyr on three ice cores from Dronning Maud Land, Antarctica 2. Seasonally resolved chemical records

TL;DR: The ammonium, calcium, and sodium concentrations from three intermediate depth ice cores drilled in the area of Dronning Maud Land, East Antarctica, have been investigated by as mentioned in this paper.
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Sulphate record from a Northeast Greenland ice core over the last 1200 years based on continuous flow analysis

TL;DR: In this article, a 150 m deep ice core from the low-accumulation area of northeast Greenland was analyzed for sulphate, calcium, sodium and electrolytical meltwater conductivity at a depth resolution of approximately 1 cm by continuous flow analysis (CFA).
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A model‐based interpretation of low‐frequency changes in the carbon cycle during the last 120,000 years and its implications for the reconstruction of atmospheric Δ14C

TL;DR: In this paper, an ocean/atmosphere/biosphere box model of the global carbon cycle (BICYCLE) was proposed to reproduce low-frequency changes in atmospheric CO2 as seen in Antarctic ice cores.