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From:Earth System Science Data (Vol. 13, Issue 8) Peer-ReviewedThe science guiding the EUREC.sup.4 A campaign and its measurements is presented. EUREC.sup.4 A comprised roughly 5 weeks of measurements in the downstream winter trades of the North Atlantic - eastward and southeastward...
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From:Atmospheric Chemistry and Physics (Vol. 16, Issue 11) Peer-ReviewedIn the framework of the Fennec international programme, a field campaign was conducted in June 2011 over the western Sahara. It led to the first observational data set ever obtained that documents the...
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From:Earth System Science Data (Vol. 13, Issue 2) Peer-ReviewedTo advance the understanding of the interplay among clouds, convection, and circulation, and its role in climate change, the Elucidating the role of clouds-circulation coupling in climate campaign (EUREC.sup.4 A) and...
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 6) Peer-ReviewedThe presence of clouds above the tropopause over tropical convection centers has so far been documented by spaceborne instruments that are either sun-synchronous or insensitive to thin cloud layers. Here we document, for...
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From:Geoscientific Model Development (Vol. 11, Issue 5) Peer-ReviewedThis paper presents the Meso-NH model version 5.4. Meso-NH is an atmospheric non hydrostatic research model that is applied to a broad range of resolutions, from synoptic to turbulent scales, and is designed for studies...
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 3) Peer-ReviewedThe amount of ice injected into the tropical tropopause layer has a strong radiative impact on climate. A companion paper (Part 1) used the amplitude of the diurnal cycle of ice water content (IWC) as an estimate of ice...
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 18) Peer-Reviewed
The source and pathway of the hydration patch in the TTL (tropical tropopause layer) that was measured during the Stratospheric and upper tropospheric processes for better climate predictions (StratoClim) field...
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 9) Peer-Reviewed
The contribution of deep convection to the amount of water vapour and ice in the tropical tropopause layer (TTL) from the tropical upper troposphere (UT; around 146 hPa) to the tropopause level (TL; around...