Results 171 to 180 of about 34,745 (260)

Transport to the Extratropical Stratosphere by Overshooting Storms in Idealized Simulations

Journal of Geophysical Research: Atmospheres, Volume 131, Issue 8, 28 April 2026.
Abstract Deep convection is a significant source of water to the extratropical stratosphere which can alter radiative properties and contribute to ozone loss. Previous studies find it responsible for 40% of mid‐latitude water vapor above 380K. However, the amount of hydration from individual storms and the mechanisms that initiate mixing is less ...
Devin P. Bissell, Christopher J. Nowotarski, Kenneth P. Bowman, Anita D. Rapp   +3 more
wiley   +1 more source

Tropics-wide intraseasonal oscillations. [PDF]

Proc Natl Acad Sci U S A
Bao J, Bony S, Takasuka D, Muller C.
europepmc   +1 more source

Atmospheric Adjustments to In Situ Cirrus Formation in Ice Supersaturated Regions

Journal of Geophysical Research: Atmospheres, Volume 131, Issue 8, 28 April 2026.
Abstract High‐level ice clouds exert a net warming on the climate system because their greenhouse effect outweighs their albedo effect. Focusing on in‐situ cirrus, their formation involves the conversion of upper‐tropospheric water vapor into ice crystals.
Jérémie Juvin‐Quarroz, Audran Borella, Patryk Kiepas, Thomas Dubos, Olivier Boucher, Nicolas Bellouin   +5 more
wiley   +1 more source

Thermo solutal convective transport of aqueous Fe₃O₄ nanofluid in an inclined porous annulus under combined thermophoretic and electrophoretic forces. [PDF]

Sci Rep
Shilpa B, Badruddin IA, Reddy RG, Kamangar S, Zuber M, Mahmoud ERI.   +5 more
europepmc   +1 more source

Field Observations Validate LES‐Derived Scaling of Vertical‐Velocity Variance During the Afternoon Transition of the Convective Boundary Layer

Geophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract The convective velocity scale is commonly used to describe the vertical‐velocity variance in the convective boundary layer driven by surface heating, and is valid when the surface heat flux varies slowly compared to the eddy turnover time. This quasi‐equilibrium assumption typically holds from late morning to early afternoon, but breaks down ...
Omar El Guernaoui, Dan Li, Radouan Boukharfane   +2 more
wiley   +1 more source

Quasi‐Stationary Atmospheric Rivers as the Primary Driver of Rossby Wave Activity in the Global Subtropics

Geophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract Hovmöller plots of upper‐tropospheric local (Rossby) wave activity (LWA) show that the subtropics of the North Pacific/Atlantic basins are relatively wave‐free in the upstream and wavier in the downstream of quasi‐stationary atmospheric rivers (QSARs).
Hung‐I. Lee, Noboru Nakamura
wiley   +1 more source

The Third Skin: A Biomimetic Hydronic Conditioning System, a New Direction in Ecologically Sustainable Design. [PDF]

Biomimetics (Basel)
Luther MB, Hyde R, Gamage A, Do HQ.
europepmc   +1 more source

The physiology of survival: Heat

Experimental Physiology, Volume 111, Issue 5, Page 2397-2402, 1 May 2026.
Josh Foster, Robert D. Meade, Tom Matthews   +2 more
wiley   +1 more source

3D‐Printed Geopolymer as a Basic Heterogeneous Catalyst for the Synthesis of α‐Cyanoacrylates Through the Knoevenagel Condensation

European Journal of Organic Chemistry, Volume 29, Issue 16, 25 April 2026.
3D‐printed geopolymers are presented as efficient and reusable heterogeneous catalysts for the Knoevenagel condensation. Under mild and green conditions, they promote the high‐yield synthesis of diverse α‐cyanoacrylates with remarkable stability and scalability.
Francesca T. Albino, Pedro A. M. Moro, Wanessa B. Menegaro, Luciano Senff, Marcus M. Sá, Dachamir Hotza   +5 more
wiley   +1 more source

Bridging heat-flow and guarded-heater methods for thermoelectric module efficiency evaluation. [PDF]

iScience
Amagai Y, Okawa K, Funahashi R, Yamamoto A, Ohta M.   +4 more
europepmc   +1 more source