Results 121 to 130 of about 4,369,447 (323)
The stratospheric gravity wave field produced by a supercell
Supercells are a class of long‐lasting thunderstorms with rotating updrafts that often cause severe weather, hail, and tornadoes. This study uses numerical simulations to characterize the stratospheric gravity waves that are caused by these storms.
David S. Nolan, Yi Dai
wiley +1 more source
Physical oceanography and current meter data from mooring AWI244-3
Gerd Rohardt, Olaf Boebel
openalex +1 more source
When tiny convective spread affects a midlatitude jet: Spread sequence
We investigate spread evolution by mesoscale convection from tiny initial condition uncertainty during a real event. There is significant variation among the systems in their propensity to interact with the jet stream, whereby variability in one system (due to convective and long‐wave radiative heating tendencies) tightly relates to Rossby‐like ...
Edward Groot, Michael Riemer
wiley +1 more source
Fundamentals of Estuarine Physical Oceanography
L. B. Miranda +3 more
semanticscholar +1 more source
Fuzzy postprocessing of seasonal climate forecasts for semiarid river basins
Meteorological forecasts from AI‐based fuzzy rule‐based system (FRB) are compared to linear scaling (LS) and quantile mapping (QM). Seasonal forecasts from the Copernicus Climate Change Service (C3S) are considered. Results show that the highest skill is achieved for the FRB approach.
Dariana Isamel Avila‐Velasquez +2 more
wiley +1 more source
Physical oceanography and current meter data from mooring AWI212
Eberhard Fahrbach, Gerd Rohardt
openalex +1 more source
Soil Moisture Active Passive soil moisture retrievals are assimilated into a land surface model and the resulting land reanalysis product is used to initialise the land component of coupled land‐atmosphere experiments. We show that the local impact of land data assimilation on the atmosphere is influenced by two factors: the magnitude by which it ...
Zdenko Heyvaert +6 more
wiley +1 more source
This study analysed and modelled summertime indoor temperature dynamics in the Netherlands using a unique long‐term crowdsourced dataset from seven residences (spanning 2–27 years). Indoor temperatures were found to rise and cool more slowly than outdoors (mean 260 minute lag), with heatwave signals persisting about five days.
Esther E. M. Peerlings +1 more
wiley +1 more source

