Results 221 to 230 of about 24,422 (290)
Lapsed El Niño impact on Atlantic and Northwest Pacific tropical cyclone activity in 2023. [PDF]
Zhao J +5 more
europepmc +1 more source
Relationships Between Great Lakes Extratropical Cyclone Characteristics and Global Teleconnections
Abstract The Great Lakes Region sits at the intersection of multiple North American storm tracks. During the cold season (October–March), the regional weather is dominated by extratropical cyclone activity. While these Great Lakes extratropical cyclones (GL ETCs) are getting warmer and holding more moisture with time, there is considerable interannual ...
Abby Hutson +4 more
wiley +1 more source
Leading role of Saharan dust on tropical cyclone rainfall in the Atlantic Basin. [PDF]
Zhu L +4 more
europepmc +1 more source
Abstract Tornadic tropical cyclones (TCs) in China occur at a similar frequency to those in the U.S., yet the number of TC tornadoes in China is only 16.5% of that in the U.S. This study reveals that one reason is that tornadic TCs in China have shorter track lengths, fewer recurving tracks, and more southerly locations when producing tornadoes.
Jingyi Wen +3 more
wiley +1 more source
Impact-based forecasting of tropical cyclone-related human displacement to support anticipatory action. [PDF]
Kam PM +5 more
europepmc +1 more source
On the Forecast Errors of Tropical Cyclone Intensity in HWRF Over the Western North Pacific
Abstract Intensity forecast errors of tropical cyclones (TCs) over the western North Pacific are investigated using forecast records from the Hurricane Weather Research and Forecasting (HWRF) model. Intensity errors increase with the lead time, growing most rapidly during the first 36 hr.
Hao‐Yan Liu, Zhe‐Min Tan
wiley +1 more source
Tropical cyclone activity over western North Pacific favors Arctic sea ice increase. [PDF]
Zeng L +9 more
europepmc +1 more source
Growth Rate and Energy Dissipation in Wind‐Forced Breaking Waves
Abstract We investigate the energy growth and dissipation of wind‐forced breaking waves at high wind speed using direct numerical simulations of the coupled air–water Navier–Stokes equations. A turbulent wind boundary layer drives the growth of a pre‐existing narrowband wave field until it breaks, transferring energy into the water column.
Nicolò Scapin +5 more
wiley +1 more source
Decreasing global tropical cyclone frequency in CMIP6 historical simulations. [PDF]
Zhao H +6 more
europepmc +1 more source

