Analysis of Coastal Fog from a Ship During the C-FOG Campaign

Author(s):  
S. Wang ◽  
H. J. S. Fernando ◽  
C. Dorman ◽  
E. Creegan ◽  
R. Krishnamurthy ◽  
...  
Keyword(s):  
2014 ◽  
Vol 141 (690) ◽  
pp. 1894-1905 ◽  
Author(s):  
Driss Bari ◽  
Thierry Bergot ◽  
Mohamed El Khlifi
Keyword(s):  

Author(s):  
Reneta Dimitrova ◽  
Ashish Sharma ◽  
Harindra J. S. Fernando ◽  
Ismail Gultepe ◽  
Ventsislav Danchovski ◽  
...  

2018 ◽  
Vol 18 (1) ◽  
pp. 127-144 ◽  
Author(s):  
Camilo del Río ◽  
Daniela Rivera ◽  
Alexander Siegmund ◽  
Nils Wolf ◽  
Pilar Cereceda ◽  
...  

1964 ◽  
Vol 21 (2) ◽  
pp. 327-333 ◽  
Author(s):  
L. V. Worthington

An oceanographic section made with the research vessel Crawford in June 1959 showed that the proportion of Labrador-Coastal Water to Slope Water at the meridian 57°30′W was unusually large. Data from this section combined with bathythermograms taken elsewhere in the Slope Water area and direct deep current measurements suggest that there was an abnormal influx of cold water from the Labrador Basin in 1959. This suggestion is strengthened by the high incidence of coastal fog in the summer of 1959. It is suggested that the cause of this influx was an abnormal North Atlantic weather pattern in January 1959.


2020 ◽  
Author(s):  
Paola Formenti ◽  
Danitza Klopper ◽  
Servanne Chevaillier ◽  
Barbara D’Anna ◽  
Karine Desboeufs ◽  
...  

<p>The western coast of southern Africa off Namibia is characterized by a semi-permanent and widespread stratocumulus (Sc) cloud deck, very frequent coastal fog, and the oceanic northern Benguela upwelling system (nBUS). It is also the crossroad of large quantities of natural and anthropogenic aerosols of distant and local origins (biogenic, anthropogenic, biomass burning, sea salt and mineral dust) from continental and marine sources, with significant differences in terms of physico-chemical and optical properties, water affinity, scale and height of transport, which are not well represented in climate models.</p><p>In this presentation we will illustrate the results of the first extensive chemical and microphysical characterisation of aerosol particles in the area that has been conducted since 2016 at  the coastal Henties Bay experimental site (22°6’ S, 14°17’ E) in the framework of the AErosol, RadiatiOn and CLOuds in southern Africa (AEROCLO-sA) and the Atmospheric Research in the Southern Africa and Indian Ocean (ARSAIO) projects.</p><p>Synergetic filter sampling and online measurements provide examples of the numerous new particle formation in link with marine biogenic emissions and the apportionment of maritime sulfate aerosols, including their biogenic component.</p>


1978 ◽  
Vol 17 (21) ◽  
pp. 3339
Author(s):  
H. G. Hughes ◽  
D. R. Jensen
Keyword(s):  

Author(s):  
Clive E. Dorman ◽  
Andrey A. Grachev ◽  
Ismail Gultepe ◽  
Harindra J. S. Fernando
Keyword(s):  

2001 ◽  
Vol 16 (1) ◽  
pp. 31-34 ◽  
Author(s):  
Walter W. Kastner ◽  
Steve M. Dutton ◽  
David M. Roché

Abstract Douglas-fir (Pseudotsuga menziesii var. menziesii) seedlings grown from three seed sources were evaluated for 5 yr on a high-disease-hazard site for their relative tolerance to Swiss needle cast. The seed sources were: (1) seed collected from trees showing an apparent degree of tolerance to Swiss needle cast in natural stands in the coastal fog belt, (2) open-pollinated seed orchard seed collected from random single-pair crosses of parent trees in natural stands outside of the coastal fog belt, but west of the Oregon Coast Range summit, whose progeny demonstrated an apparent degree of disease tolerance in coastal Douglas-fir progeny test sites, and (3) standard reforestation seed purchased from a commercial vendor. There were no significant differences among seed sources in basal diameter and total height for all five growing seasons. Needle retention varied among seed sources over the 5 yr period, but current-year needle retention did not vary significantly after the fifth growing season, and retention of 1- and 2-yr-old needles was relatively low for all seed sources. The intense disease pressure on this site may have overwhelmed expression of disease tolerance among seed sources. We do not recommend planting Douglas-fir on such high-hazard sites. West J. Appl. For. 16(1):31–34.


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