Data Gaps within Atmospheric Rivers over the Northeastern Pacific

Atmospheric Feedbacks over the Tropical Pacific in Observations and Atmospheric General Circulation Models: An Extended Assessment

The dynamical and radiative feedbacks from the deep convection over the tropical Pacific are quantified using ENSO signal in that region for both the observation and 16 climate models. Different from a previous analysis, we recognize the nonlinear relationship between deep convection and SST over that region, and perform the evaluation using the data from the warm phase and the cold phase separ...

How Do Atmospheric Rivers Form?

Atmospheric rivers: a mini-review

*Correspondence: Luis Gimeno, EPhyslab, Departamento de Física Aplicada, Universidad de Vigo, Campus As Lagoas, 32004 Ourense, Spain e-mail: [email protected] Atmospheric rivers (ARs) are narrow regions responsible for the majority of the poleward water vapor transport across the midlatitudes. They are characterized by high water vapor content and strong low level winds, and form a part of the ...

Organic aerosols in the Northeastern Pacific

Organics in the Northeastern Pacific and their impacts on aerosol hygroscopicity in the subsaturated and supersaturated regimes K. K. Crahan, D. A. Hegg, D. S. Covert, J. L. Santarpia, H. Jonsson, G. Buzorius, and D. Collins Department of Atmospheric Sciences, Seattle, WA, USA Edgewood Chemical Biological Center, Aberdeen Proving Grounds, MD, USA CIRPAS, Department of Research, NPS, Marina, CA,...

the effect of atmospheric rivers on iran climate

introduction: water vapor spreads in molecular, unstable and erratic phase and transfers by convection and advection process. this transfer happens from the earth and oceans' surfaces to the atmosphere by the hot air. this type of this transfer is considered as the main pattern. in the studies of the atmosphere, one of the prominent factors to be considered is the complexity of water vapor...