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Preindustrial-to-present-day changes in atmospheric carbon monoxide: agreement and gaps between ice archives and global model reconstructions Atmospheric Chemistry and Physics, 2025 (Ref: 17279)
Category 1: Peer-reviewed literature

Global chemistry–climate models (CCMs) play an important role in assessing the climate and air pollution implications of aerosols and chemically reactive gases.

Preindustrial-to-present-day changes in atmospheric carbon monoxide: agreement and gaps between ice archives and global model reconstructions Atmospheric Chemistry and Physics, 2025 (Ref: 17403)
Category 1: Peer-reviewed literature

Global chemistry–climate models (CCMs) play an important role in assessing the climate and air pollution implications of aerosols and chemically reactive gases.

Predicting trends in atmospheric CO2 across the Mid-Pleistocene Transition using existing climate archives Climate of the Past, 2024 (Ref: 17203)
Category 1: Peer-reviewed literature

During the Mid-Pleistocene Transition (MPT), ca. 1200–800?000 years ago (ka), the Earth's glacial cycles changed from 41 to 100?kyr periodicity.

Reduced Deep Convection and Bottom Water Formation Due To Antarctic Meltwater in a Multi-Model Ensemble. Geophysical Research Letters, 2023 (Ref: 17125)
Category 1: Peer-reviewed literature

The additional water from the Antarctic ice sheet and ice shelves due to climate-induced melt can impact ocean circulation and global climate. However, the major processes driving melt are not adequately represented in Coupled Model Intercomparison Project phase 6 (CMIP6) models. Here…

Return of the Maud Rise Polynya: Climate litmus or sea ice anomaly? [In: State of the Climate in 2017] Bulletin of the American Meteorological Society, 2018 (Ref: 17043)
Category 1: Peer-reviewed literature

The Maud Rise polynya is a persistent area of open water within the sea ice cover of the Southern Ocean, which overlies an area of elevated topography called Maud Rise (66°S, 3°E) located in the eastern sector of the Weddell Sea (Fig. SB6.1a).

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