World's Best Scientists 2026 revealed!

D-Index & Metrics

Environmental Sciences

D-Index
36
Citations
6822
World Ranking
9074
National Ranking
208

Overview

What is he best known for?

The fields of study he is best known for:

  • Climate change
  • Global warming
  • Oceanography

The scientist’s investigation covers issues in Ice core, Oceanography, Carbon cycle, Isotopes of carbon and Environmental science. Jochen Schmitt interconnects Glacial period, Ice sheet and European Project for Ice Coring in Antarctica in the investigation of issues within Ice core. His study in Glacial period is interdisciplinary in nature, drawing from both Sea ice, Meteorology and Atmospheric methane.

His studies deal with areas such as Oceanic climate and Interglacial as well as Carbon cycle. The Interglacial study combines topics in areas such as Sediment, Ice age, Carbon dioxide in Earth's atmosphere and Holocene. His Isotopes of carbon research is multidisciplinary, incorporating perspectives in Deep sea, Sea surface temperature, Deglaciation, Ocean current and Last Glacial Maximum.

His most cited work include:

  • One-to-one coupling of glacial climate variability in Greenland and Antarctica. (920 citations)
  • Carbon Isotope Constraints on the Deglacial CO2 Rise from Ice Cores (265 citations)
  • Carbon Isotope Constraints on the Deglacial CO2 Rise from Ice Cores (265 citations)

What are the main themes of his work throughout his whole career to date?

His scientific interests lie mostly in Ice core, Environmental science, Atmospheric sciences, Interglacial and Glacial period. His Ice core research includes elements of Carbon cycle, Holocene and Isotopes of carbon. His work in Isotopes of carbon covers topics such as Analytical chemistry which are related to areas like Isotope analysis.

His Atmospheric sciences research includes themes of Hydrology, Permafrost and Last Glacial Maximum. Jochen Schmitt has researched Interglacial in several fields, including Sediment, Sea level, Deglaciation and Earth science. He combines subjects such as Isotopic composition, Climate change and Dome with his study of Glacial period.

He most often published in these fields:

  • Ice core (83.61%)
  • Environmental science (34.97%)
  • Atmospheric sciences (33.88%)

What were the highlights of his more recent work (between 2019-2021)?

  • Ice core (83.61%)
  • Interglacial (41.53%)
  • Environmental science (34.97%)

In recent papers he was focusing on the following fields of study:

Ice core, Interglacial, Environmental science, Atmospheric sciences and Glacial period are his primary areas of study. His research integrates issues of Deglaciation, Holocene, Sea level, Ice sheet and Atmospheric methane in his study of Ice core. His Interglacial study incorporates themes from Climatology, Ocean heat content and Sea surface temperature.

In his study, which falls under the umbrella issue of Climatology, Land ice, Carbon cycle and Atmosphere is strongly linked to Intertropical Convergence Zone. Ocean heat content is a primary field of his research addressed under Oceanography. Within one scientific family, Jochen Schmitt focuses on topics pertaining to Greenhouse gas under Atmospheric sciences, and may sometimes address concerns connected to Permafrost, Dome and Geomorphology.

Between 2019 and 2021, his most popular works were:

  • Preindustrial 14CH4 indicates greater anthropogenic fossil CH4 emissions. (40 citations)
  • Old carbon reservoirs were not important in the deglacial methane budget (19 citations)
  • Global ocean heat content in the Last Interglacial (8 citations)

In his most recent research, the most cited papers focused on:

  • Climate change
  • Global warming
  • Greenhouse gas

Jochen Schmitt mainly focuses on Climatology, Interglacial, Ice core, Land ice and Carbon cycle. In his papers, Jochen Schmitt integrates diverse fields, such as Ice core and Environmental science. His biological study spans a wide range of topics, including Intertropical Convergence Zone, Glacial period, Atmosphere and Before Present.

The various areas that Jochen Schmitt examines in his Deglaciation study include Atmospheric circulation, δ13C, Sea surface temperature and Mean radiant temperature. In his study, Ocean heat content is inextricably linked to Sea level, which falls within the broad field of Atmospheric circulation. His Greenhouse gas study integrates concerns from other disciplines, such as Mud volcano and Ice sheet.

Best Publications

  • One-to-one coupling of glacial climate variability in Greenland and Antarctica.

    C. Barbante;J.-M. Barnola;J.-M. Barnola;S. Becagli;J. Beer;J. Beer

  • Revision of the EPICA Dome C CO2 record from 800 to 600 kyr before present

    Bernhard Bereiter;Bernhard Bereiter;Bernhard Bereiter;Sarah Skye Eggleston;Sarah Skye Eggleston;Jochen Schmitt;Jochen Schmitt;Christoph Nehrbass-Ahles;Christoph Nehrbass-Ahles

  • Carbon Isotope Constraints on the Deglacial CO2 Rise from Ice Cores

    Jochen Schmitt;Jochen Schmitt;Robert Schneider;Joachim Elsig;Daiana Leuenberger

  • Preindustrial 14CH4 indicates greater anthropogenic fossil CH4 emissions.

    Benjamin Hmiel;V. V. Petrenko;M. N. Dyonisius;C. Buizert

  • A 156 kyr smoothed history of the atmospheric greenhouse gases CO 2 , CH 4 , and N 2 O and their radiative forcing

    Peter Köhler;Christoph Nehrbass-Ahles;Jochen Schmitt;Thomas F. Stocker

  • Stable isotope constraints on Holocene carbon cycle changes from an Antarctic ice core

    Joachim Elsig;Joachim Elsig;Jochen Schmitt;Jochen Schmitt;Jochen Schmitt;Daiana Leuenberger;Daiana Leuenberger;Robert Schneider;Robert Schneider

  • Climate Change and the Integrity of Science

    Jennifer Sills;P. H. Gleick;R. M. Adams;R. M. Amasino

  • Changing boreal methane sources and constant biomass burning during the last termination

    Hubertus Fischer;Melanie Behrens;Michael Bock;Ulrike Richter

  • An improved continuous flow analysis system for high-resolution field measurements on ice cores.

    Patrik R. Kaufmann;Urs Federer;Manuel A. Hutterli;Matthias Bigler

  • The role of Southern Ocean processes in orbital and millennial CO2 variations – A synthesis

    Hubertus Fischer;Hubertus Fischer;Hubertus Fischer;Jochen Schmitt;Jochen Schmitt;Jochen Schmitt;Dieter Lüthi;Dieter Lüthi;Thomas F. Stocker;Thomas F. Stocker

  • A reconstruction of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the last glacial inception

    Robert Schneider;Robert Schneider;Jochen Schmitt;Jochen Schmitt;Jochen Schmitt;P. Köhler;Fortunat Joos;Fortunat Joos

  • Evolution of the stable carbon isotope composition of atmospheric CO2 over the last glacial cycle

    S. Eggleston;S. Eggleston;J. Schmitt;J. Schmitt;B. Bereiter;B. Bereiter;R. Schneider;R. Schneider

  • Amount-dependent isotopic fractionation during compound-specific isotope analysis.

    Jochen Schmitt;Bruno Glaser;Wolfgang Zech

  • Atmospheric Methane: Comparison Between Methane's Record in 2006–2022 and During Glacial Terminations

    Unknown

  • Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations

    Julia Gottschalk;Julia Gottschalk;Gianna Battaglia;Hubertus Fischer;Thomas L. Frölicher

  • Earth's radiative imbalance from the Last Glacial Maximum to the present.

    Daniel Baggenstos;Marcel Häberli;Jochen Schmitt;Sarah A. Shackleton

  • Atmospheric δ13CO2 and its relation to pCO2 and deep ocean δ13C during the late Pleistocene

    Peter Köhler;Hubertus Fischer;Hubertus Fischer;Jochen Schmitt;Jochen Schmitt

  • Hydrogen Isotopes Preclude Marine Hydrate CH4 Emissions at the Onset of Dansgaard-Oeschger Events

    Michael Bock;Michael Bock;Jochen Schmitt;Jochen Schmitt;LarsMöller Möller;Renato Spahni

  • High-resolution interpolar difference of atmospheric methane around the Last Glacial Maximum

    M. Baumgartner;M. Baumgartner;A. Schilt;A. Schilt;O. Eicher;O. Eicher;J. Schmitt;J. Schmitt

  • Global ocean heat content in the Last Interglacial

    S. Shackleton;D. Baggenstos;J. A. Menking;M. N. Dyonisius

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

    Michael Bock;Jochen Schmitt;Jonas Beck;Barbara Seth

  • A reconstruction of atmospheric carbon dioxide and its stable carbon isotopic composition from the penultimate glacial maximum to the glacial inception

    Robert Schneider;Jochen Schmitt;Peter Koehler;Fortunat Joos

Frequent Co-Authors

Hubertus Fischer
Hubertus Fischer University of Bern
Thomas F. Stocker
Thomas F. Stocker University of Bern
Peter Köhler
Peter Köhler Alfred Wegener Institute for Polar and Marine Research
Fortunat Joos
Fortunat Joos University of Bern
Renato Spahni
Renato Spahni University of Bern
Jérôme Chappellaz
Jérôme Chappellaz École Polytechnique Fédérale de Lausanne
Edward J. Brook
Edward J. Brook Oregon State University
Todd Sowers
Todd Sowers Pennsylvania State University
Thomas Blunier
Thomas Blunier University of Copenhagen
Markus Leuenberger
Markus Leuenberger University of Bern

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