Zobrazeno 1 - 10
of 55
pro vyhledávání: '"ddc:551.5"'
Autor:
Kumar Sahu, Rajesh, Choudhury, Goutam, Vissa, Naresh Krishna, Tyagi, Bhishma, Nayak, Sridhara
El-Niño and La-Niña are believed to change the intensity and frequencies of extreme weather events globally. The present study aims to analyse the impact of El-Niño and La-Niña on the lightning activities of cloud systems and their associated pre
Externí odkaz:
https://ul.qucosa.de/id/qucosa%3A88482
https://ul.qucosa.de/api/qucosa%3A88482/attachment/ATT-0/
https://ul.qucosa.de/api/qucosa%3A88482/attachment/ATT-0/
Autor:
Gaudek, Tom
Microphysical properties of precipitating hydrometeors, such as size, concentration, or shape, can be retrieved by vertically-resolved remote-sensing measurements. For a thorough quality assessment, a direct evaluation of those retrievals is required
Externí odkaz:
https://ul.qucosa.de/id/qucosa%3A94195
https://ul.qucosa.de/api/qucosa%3A94195/attachment/ATT-0/
https://ul.qucosa.de/api/qucosa%3A94195/attachment/ATT-0/
This study investigates the lifetime and temporal evolution of physical properties of trade‐wind cumuli based on tracking individual clouds in observations with the Advanced Baseline Imager aboard the geostationary GOES‐16 satellite during the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2497::af387f44f184b491de0c8b6b2153e7aa
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10849
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10849
The dryness of the stratosphere is the result of air entering through the cold tropical tropopause layer (TTL). However, our understanding of the moisture flux partitioning into water vapor and frozen hydrometeors is incomplete. This raises concerns
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2497::a71ce2e43aa61c36bbcd7f1d84e40f42
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10876
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10876
Autor:
Hoffmann, Fabian, Feingold, Graham
The processing of aerosol by droplet collision‐coalescence is analyzed in three‐dimensional simulations of drizzling stratocumulus using a Lagrangian cloud model for the representation of aerosol and cloud microphysics. Collision‐coalescence pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2497::3dd07b8da59485b897b5b9949b9e5f01
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10921
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10921
Autor:
Savre, Julien, Craig, George
Publikováno v:
Journal of Advances in Modeling Earth Systems. 15
Whereas it is now widely accepted that cumulus cloud sizes are power‐law distributed, characteristic exponents reported in the literature vary greatly, generally taking values between 1 and >3. Although these differences might be explained by varia
Publikováno v:
Quarterly Journal of the Royal Meteorological Society.
For both the meso‐ and synoptic scales, reduced mathematical models give insight into their dynamical behaviour. For the mesoscale, the weak temperature gradient approximation is one of several approaches, while for the synoptic scale the quasigeos
We used the tropospheric and lower stratospheric 3D winds for four consecutive years (2017–2020) to study the momentum flux (MF) and vertical wind power spectra (VWP) over Andøya, Norway (69.30°N, 16.04°E) using the Middle Atmosphere Alomar Rada
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e671d3bd60ca0dc23e47bd1af76cf03a
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10919
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10919
Autor:
Poblet, Facundo L., Vierinen, Juha, Avsarkisov, Victor, Conte, J. Federico, Charuvil Asokan, Harikrishnan, Jacobi, Christoph, Chau, Jorge L., 2 Arctic University of Norway Tromsø Norway, 1 Leibniz Institute of Atmospheric Physics at the University of Rostock Kühlungsborn Germany, 3 Institute for Meteorology Leipzig University Leipzig Germany
Measurements of kinetic energy in vortical and divergent fluctuations in the mesosphere and lower thermosphere can be used to study stratified turbulence (ST) and gravity waves. This can be done using horizontal correlation functions of the fluctuati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e6e52d83560eb52a5200e8336ce75648
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10759
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10759
Autor:
Julia Mindlin, Linda Van Garderen
Publikováno v:
van Garderen, L.; Mindlin, J.: A storyline attribution of the 2011/2012 drought in Southeastern South America. In: Weather. Vol. 77 (2022) 6, 212-218. (DOI: /10.1002/wea.4185)
The 2011/2012 summer drought in Southeastern South America (SESA) was a short but devastating event. What would this event have looked like under pre‐industrial conditions, or in a +2 degC world? We find that climate change causes the region to be