Results 21 to 30 of about 700 (138)

Observations of ozone-poor air in the tropical tropopause layer [PDF]

open access: yesAtmospheric Chemistry and Physics, 2018
Ozonesondes reaching the tropical tropopause layer (TTL) over the west Pacific have occasionally measured layers of very low ozone concentrations – less than 15 ppbv – raising the question of how prevalent such layers are and how they are formed.
R. Newton   +8 more
doaj   +1 more source

Weakening of the tropical tropopause layer cold trap with global warming [PDF]

open access: yesAtmospheric Chemistry and Physics, 2023
Lagrangian trajectories have previously been used to reconstruct water vapor variability in the lower stratosphere, where the sensitivity of surface radiation to changes in the water vapor concentration is strongest, by obtaining temperature histories of
S. Bourguet, M. Linz, M. Linz
doaj   +1 more source

Modelling deep convection and its impacts on the tropical tropopause layer [PDF]

open access: yesAtmospheric Chemistry and Physics, 2010
The UK Met Office's Unified Model is used at a climate resolution (N216, ~0.83°×~0.56°, ~60 km) to assess the impact of deep tropical convection on the structure of the tropical tropopause layer (TTL). We focus on the potential for
J. S. Hosking   +3 more
doaj   +1 more source

Effect of tropical cyclones on the stratosphere–troposphere exchange observed using satellite observations over the north Indian Ocean [PDF]

open access: yesAtmospheric Chemistry and Physics, 2016
Tropical cyclones play an important role in modifying the tropopause structure and dynamics as well as stratosphere–troposphere exchange (STE) processes in the upper troposphere and lower stratosphere (UTLS) region. In the present study, the impact of
M. Venkat Ratnam   +5 more
doaj   +1 more source

A numerical study of convective-scale downdrafts in the outer core of tropical cyclones in vertically varying environmental flows

open access: yesTropical Cyclone Research and Review, 2020
The characteristics of convective-scale downdrafts in the outer core of tropical cyclones in the lower- and upper-layer vertical wind shear (VWS) are investigated based on two high-resolution idealized numerical experiments.
Jingjing Cheng, Qingqing Li
doaj   +1 more source

The Tropical Tropopause Layer 1960–2100 [PDF]

open access: yesAtmospheric Chemistry and Physics, 2009
The representation of the Tropical Tropopause Layer (TTL) in 13 different Chemistry Climate Models (CCMs) designed to represent the stratosphere is analyzed. Simulations for 1960–2005 and 1980–2100 are analyzed.
A. Gettelman   +17 more
doaj  

Radio occultation bending angle anomalies during tropical cyclones [PDF]

open access: yesAtmospheric Measurement Techniques, 2011
The tropical deep convection affects the radiation balance of the atmosphere changing the water vapor mixing ratio and the temperature of the upper troposphere lower stratosphere.
R. Biondi   +3 more
doaj   +1 more source

The Troposphere-to-Stratosphere Transport Caused by a Rossby Wave Breaking Event over the Tibetan Plateau in Mid-March 2006

open access: yesRemote Sensing, 2022
Based on reanalysis data, satellite ozone concentration observations, and a Lagrangian trajectory simulation, a Rossby wave breaking (RWB) event and its effect on stratosphere–troposphere exchange (STE) over the Tibetan Plateau in mid-March 2006 were ...
Jinyao Zhu   +3 more
doaj   +1 more source

The influence of the Asian summer monsoon on volcanic aerosol transport in the UTLS region

open access: yesnpj Climate and Atmospheric Science, 2023
This study analyses the influence of the Asian summer monsoon on volcanic aerosol transport. Realistic, altitude-resolved SO2 emissions of a middle-latitude volcanic eruption (Sarychev 2009) and a tropical volcanic eruption (Nabro 2011) were retrieved ...
Xue Wu   +7 more
doaj   +1 more source

Linking uncertainty in simulated Arctic ozone loss to uncertainties in modelled tropical stratospheric water vapour [PDF]

open access: yesAtmospheric Chemistry and Physics, 2018
Stratospheric water vapour influences the chemical ozone loss in the polar stratosphere via control of the polar stratospheric cloud formation. The amount of water vapour entering the stratosphere through the tropical tropopause differs substantially ...
L. Thölix   +3 more
doaj   +1 more source

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