near surface
Recently Published Documents


TOTAL DOCUMENTS

15208
(FIVE YEARS 5662)

H-INDEX

143
(FIVE YEARS 38)

2022 ◽  
Vol 236 ◽  
pp. 111534
Author(s):  
Andreas Fell ◽  
Johannes Greulich ◽  
Frank Feldmann ◽  
Christoph Messmer ◽  
Jonas Schön ◽  
...  

Geoderma ◽  
2022 ◽  
Vol 410 ◽  
pp. 115661
Author(s):  
Hyoun Soo Lim ◽  
Hyun-Cheol Kim ◽  
Ok-Sun Kim ◽  
Hyejung Jung ◽  
Jeonghoon Lee ◽  
...  

2022 ◽  
Vol 266 ◽  
pp. 105948
Author(s):  
Cheng Shen ◽  
Jinlin Zha ◽  
Jian Wu ◽  
Deming Zhao ◽  
Cesar Azorin-Molina ◽  
...  

2022 ◽  
Vol 243 ◽  
pp. 106796
Author(s):  
Josh Wimpenny ◽  
Gary R. Eppich ◽  
Naomi Marks ◽  
Frederick Ryerson ◽  
Kim B. Knight

2022 ◽  
Vol 114 ◽  
pp. 103561
Author(s):  
Léna Rossi ◽  
Corinne Loisy ◽  
Adrian Cerepi ◽  
Anélia Petit ◽  
Olivier Le Roux ◽  
...  

Atmosphere ◽  
2022 ◽  
Vol 13 (1) ◽  
pp. 138
Author(s):  
Yu Wang ◽  
Corene J. Matyas

This study examined whether varying moisture availability and roughness length for the land surface under a simulated Tropical Cyclone (TC) could affect its production of precipitation. The TC moved over the heterogeneous land surface of the southeastern U.S. in the control simulation, while the other simulations featured homogeneous land surfaces that were wet rough, wet smooth, dry rough, and dry smooth. Results suggest that the near-surface atmosphere was modified by the changes to the land surface, where the wet cases have higher latent and lower sensible heat flux values, and rough cases exhibit higher values of friction velocity. The analysis of areal-averaged rain rates and the area receiving low and high rain rates shows that simulations having a moist land surface produce higher rain rates and larger areas of low rain rates in the TC’s inner core. The dry and rough land surfaces produced a higher coverage of high rain rates in the outer regions. Key differences among the simulations happened as the TC core moved over land, while the outer rainbands produced more rain when moving over the coastline. These findings support the assertion that the modifications of the land surface can influence precipitation production within a landfalling TC.


Sign in / Sign up

Export Citation Format

Share Document