Zobrazeno 1 - 10
of 33
pro vyhledávání: '"V. A. Sinclair"'
Publikováno v:
Geoscientific Model Development, Vol 17, Pp 2961-2986 (2024)
This article presents a description of an analytical, stable, and flexible initial background state for both dry and moist baroclinic wave simulation on an aquaplanet in order to test the dynamical core of numerical weather prediction models and stud
Externí odkaz:
https://doaj.org/article/be97f7660a1d4b4394c8ec827736ea35
Autor:
V. A. Sinclair, J. L. Catto
Publikováno v:
Weather and Climate Dynamics, Vol 4, Pp 567-589 (2023)
Extra-tropical cyclones (ETCs) are the main cause of precipitation in the mid-latitudes, and there is substantial evidence that ETC-related precipitation will increase in the future. However, little is known about how this will impact on the dynamica
Externí odkaz:
https://doaj.org/article/f36eb0dc1892438c950a283ef6577446
Publikováno v:
Atmospheric Chemistry and Physics, Vol 23, Pp 821-842 (2023)
Local along-valley winds in four major valleys on the southern slope of the Nepal Himalayas are studied by means of high-resolution meteorological modelling. The Weather Research and Forecasting model is run with a 1 km horizontal grid spacing coveri
Externí odkaz:
https://doaj.org/article/80022bdc3a024df6bade1038ab78d68f
Publikováno v:
Atmospheric Measurement Techniques, Vol 15, Pp 3075-3103 (2022)
We investigate the boundary-layer (BL) height at Hyytiälä in southern Finland diagnosed from radiosonde observations, a microwave radiometer (MWR) and ERA5 reanalysis. Four different, pre-existing algorithms are used to diagnose the BL height from
Externí odkaz:
https://doaj.org/article/f07a439b1a79481c809dd0ddb9c853e8
Autor:
D. Aliaga, V. A. Sinclair, M. Andrade, P. Artaxo, S. Carbone, E. Kadantsev, P. Laj, A. Wiedensohler, R. Krejci, F. Bianchi
Publikováno v:
Atmospheric Chemistry and Physics, Vol 21, Pp 16453-16477 (2021)
Observations of aerosol and trace gases in the remote troposphere are vital to quantify background concentrations and identify long-term trends in atmospheric composition on large spatial scales. Measurements made at high altitude are often used to s
Externí odkaz:
https://doaj.org/article/5234d5523c6e4b119958246604b2b908
Publikováno v:
Weather and Climate Dynamics, Vol 2, Pp 1111-1130 (2021)
Extratropical cyclones play a major role in the atmospheric circulation and weather variability and can cause widespread damage and destruction. Extratropical cyclones in northern Europe, which is located at the end of the North Atlantic storm track,
Externí odkaz:
https://doaj.org/article/be87ac4c299448ff8438849208a10f28
Publikováno v:
Weather and Climate Dynamics, Vol 1, Pp 1-25 (2020)
Little is known about how the structure of extra-tropical cyclones will change in the future. In this study aqua-planet simulations are performed with a full-complexity atmospheric model. These experiments can be considered an intermediate step towar
Externí odkaz:
https://doaj.org/article/a9e358ca574f49fab297130ab83d5e1d
Publikováno v:
Atmospheric Chemistry and Physics, Vol 19, Pp 1985-2000 (2019)
The presence of clouds and their characteristics have a strong impact on the radiative balance of the Earth and on the amount of solar radiation reaching the Earth's surface. Many applications require accurate forecasts of surface radiation on weathe
Externí odkaz:
https://doaj.org/article/8be23bab410a46708343ec5d5109ca90
Publikováno v:
Geoscientific Model Development, Vol 10, Iss 2, Pp 827-841 (2017)
A software package (OZO, Omega–Zwack–Okossi) was developed to diagnose the processes that affect vertical motions and geopotential height tendencies in weather systems simulated by the Weather Research and Forecasting (WRF) model. First, this sof
Externí odkaz:
https://doaj.org/article/d19fbae278c2499dad1e21f31fa1b67b
Autor:
L. Riuttanen, M. Bister, V.-M. Kerminen, V. O. John, A.-M. Sundström, M. Dal Maso, J. Räisänen, V. A. Sinclair, R. Makkonen, F. Xausa, G. de Leeuw, M. Kulmala
Publikováno v:
Atmospheric Chemistry and Physics, Vol 16, Pp 14331-14342 (2016)
Aerosol–cloud interactions are the largest source of uncertainty in the radiative forcing of the global climate. A phenomenon not included in the estimates of the total net forcing is the potential increase in upper tropospheric humidity (UTH) b
Externí odkaz:
https://doaj.org/article/b78b6c1cd7da4541a31dccaedcb63576