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11.
GPS for weather and space weather studies
Andreja Sušnik, 2013, doktorska disertacija

Najdeno v: ključnih besedah
Povzetek najdenega: ...elektromagnetni valovi, propagacija, atmosfera, GPS, Ramanski lidar, atmosferska vodna para, atmosferski zamiki signalov, mešalno...
Ključne besede: elektromagnetni valovi, propagacija, atmosfera, GPS, Ramanski lidar, atmosferska vodna para, atmosferski zamiki signalov, mešalno razmerje vodne pare, ionosferske fluktuacije, kozmični žarki, topografija, disertacije
Objavljeno: 25.04.2014; Ogledov: 2728; Prenosov: 34
URL Polno besedilo (0,00 KB)
Gradivo ima več datotek! Več...

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Combined measurments of water vapor over Vipava Valley, Slovenia
Andreja Sušnik, Tingyao He, Fei Gao, Klemen Bergant, Samo Stanič, Darko Veberič, 2013, objavljeni povzetek znanstvenega prispevka na konferenci

Najdeno v: ključnih besedah
Povzetek najdenega: ...atmosferska fizika, vodna para, Mie lidar, GPS, radiosonde, ...
Ključne besede: atmosferska fizika, vodna para, Mie lidar, GPS, radiosonde
Objavljeno: 22.01.2015; Ogledov: 2754; Prenosov: 67
URL Polno besedilo (0,00 KB)

13.
Observations of atmospheric structures in the Vipava valley based on Lidar data
Klemen Bergant, William Eichinger, Samo Stanič, Asta Gregorič, Longlong Wang, Maruška Mole, Marko Vučković, 2016, objavljeni povzetek znanstvenega prispevka na konferenci

Najdeno v: ključnih besedah
Ključne besede: lidar, atmosferske strukture, vremenske razmere
Objavljeno: 03.05.2016; Ogledov: 2166; Prenosov: 0
.pdf Polno besedilo (33,19 KB)

14.
Evolution of the planetary boundary layer in the presence of fog and plume
Maruška Mole, Marko Vučković, Klemen Bergant, Asta Gregorič, Samo Stanič, Longlong Wang, 2016, objavljeni povzetek znanstvenega prispevka na konferenci

Najdeno v: ključnih besedah
Povzetek najdenega: ... lidar, vodna para, sipanje, GPS...
Ključne besede: lidar, vodna para, sipanje, GPS
Objavljeno: 03.05.2016; Ogledov: 2385; Prenosov: 1
.pdf Polno besedilo (35,71 KB)

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Lidar measurements of Bora wind effects on aerosol loading
Maruška Mole, Longlong Wang, Samo Stanič, Klemen Bergant, William Eichinger, Francisco Ocaña, Benedikt Strajnar, Primož Škraba, Marko Vučković, William Willis, 2017, izvirni znanstveni članek

Opis: The Vipava valley in Slovenia is well known for the appearance of strong, gusty North-East Bora winds, which occur as a result of air flows over an adjacent orographic barrier. There are three revealing wind directions within the valley which were found to give rise to specific types of atmospheric structures. These structures were investigated using a Mie scattering lidar operating at 1064 nm, which provided high temporal and spatial resolution backscatter data on aerosols, which were used as tracers for atmospheric flows. Wind properties were monitored at the bottom of the valley and at the rim of the barrier using two ultrasonic anemometers. Twelve time periods between February and April 2015 were selected when lidar data was available. The periods were classified according to the wind speed and direction and investigated in terms of appearance of atmospheric structures. In two periods with strong or moderate Bora, periodic atmospheric structures in the lidar data were observed at heights above the mountain barrier and are believed to be Kelvin–Helmholtz waves, induced by wind shear. No temporal correlation was found between these structures and wind gusts at the ground level. The influence of the wind on the height of the planetary boundary layer was studied as well. In periods with low wind speeds, the vertical evolution of the planetary boundary layer was found to be governed by solar radiation and clouds. In periods with strong or moderate Bora wind, convection within the planetary boundary layer was found to be much weaker due to strong turbulence close to the ground, which inhibited mixing through the entire layer.
Najdeno v: ključnih besedah
Ključne besede: Downslope wind Lidar observations Kelvin–Helmholtz waves Bora
Objavljeno: 06.01.2017; Ogledov: 2107; Prenosov: 0
.pdf Polno besedilo (3,02 MB)

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Zakaj je burja najmočnejša v Vipavski dolini?
Samo Stanič, 2017, intervju

Opis: Ste se kdaj spraševali, zakaj je burja pri nas najmočnejša prav v Vipavski dolini? "Kriva" je pravzaprav reliefna slika Vipavske doline: burja je namreč pojav, ki nastane na zavetrni strani gorskih verig, kjer zaradi toka hladnega zraka čez oviro nastanejo močni pobočni vetrovi. Pojav je povezan s prisotnostjo toplih zračnih mas v nižinah JZ Slovenije in stabilnih hladnih zračnih mas nad osrednjo Slovenijo, ki se ob gorski pregradi prelivajo v dolino. Razgiban relief JZ Slovenije, ki se v manj kot tridesetih kilometrih preko Kraške planote in Vipavske doline dvigne na planoto Trnovskega gozda tudi s 1500 m nadmorske višine namreč omogoča razvoj burje v Vipavski dolini, katere poglavitna značilnost so močni sunki.
Najdeno v: ključnih besedah
Povzetek najdenega: ...burja, daljinsko zaznavanje, lidar, Vipavska dolina...
Ključne besede: burja, daljinsko zaznavanje, lidar, Vipavska dolina
Objavljeno: 05.03.2018; Ogledov: 1562; Prenosov: 0
.pdf Polno besedilo (2,88 MB)

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