scholarly journals A Long-Term Assessment of the Black Sea Wave Climate

2017 ◽  
Vol 9 (10) ◽  
pp. 1875 ◽  
Author(s):  
Florin Onea ◽  
Liliana Rusu
Keyword(s):  
Black Sea ◽  
Wave Climate ◽  
The Black Sea ◽  
Sea Wave

scholarly journals ASSESSMENT OF LONG-TERM WIND AND WAVE TRENDS IN THE BLACK SEA

2020 ◽  
pp. 5
Author(s):  
Fulya Islek ◽  
Yalcin Yuksel ◽  
Cihan Sahin
Keyword(s):  
Climate Change ◽  
Black Sea ◽  
Wave Climate ◽  
The Black Sea ◽  
Wind Fields ◽  
Wave Characteristics ◽  
Wind Characteristics ◽  
Mike 21 Sw ◽  
Mike 21

The wind and wave climate over the Black Sea were investigated by providing extensive datasets covering the last 40 years (1979-2018). Wind characteristics over the Black Sea were evaluated by using two well-known wind fields (i.e., ECMWF ERA-Interim and NCEP/CFSR). Wave simulations were generated from the MIKE 21 SW model forcing with two wind datasets. The possible effect of the long-term variability on the wind and wave characteristics over the Black Sea was discussed in the context of climate change.

LONG-TERM AND EXTREME WAVE CLIMATE OF THE BLACK SEA

2005 ◽  
Author(s):  
ERDAL OZHAN ◽  
SALEH ABDALLA ◽  
NIHAL YILMAZ
Keyword(s):  
Black Sea ◽  
Wave Climate ◽  
The Black Sea ◽  
Extreme Wave

scholarly journals Methods of Analyzing Nonstationary Variability of the Black Sea Wave Climate

2018 ◽  
Vol 25 (4) ◽  
Author(s):  
Ya. V. Saprykina ◽  
S. Yu. Kuznetsov ◽  
◽  
Keyword(s):  
Black Sea ◽  
Wave Climate ◽  
The Black Sea ◽  
Sea Wave

Oithona davisae: naturalization in the Black sea, inter-annual and seasonal dynamics, effect on the structure of the planktonic copepod community

2019 ◽  
Vol 59 (6) ◽  
pp. 1008-1015
Author(s):  
A. D. Gubanova ◽  
O. A. Garbazey ◽  
D. A. Altukhov ◽  
V. S. Mukhanov ◽  
E. V. Popova
Keyword(s):  
Black Sea ◽  
Coastal Waters ◽  
Native Species ◽  
Significant Decline ◽  
Acartia Tonsa ◽  
The Black Sea ◽  
Copepod Community ◽  
Oithona Davisae ◽  
Sevastopol Bay

Long-term (20032014) routine observations of zooplankton in Sevastopol Bay (the Black Sea) have allowed the naturalization of the invasive copepod Oithona davisae to be studied in the Black Sea coastal waters. Inter-annual and seasonal variability of the species and their impact on the native copepod community have been analyzed. The invasion of O. davisae and their undoubted dominance in terms of abundance were shown to alter the community structure but, at the same time, the abundances of the native species did not decrease, excepting the Black Sea earlier invader Acartia tonsa. A significant decline in A. tonsa numbers over the stages of O. davisae establishment and naturalization provided evidence of competition between the species. O. davisae have been demonstrated to gain competitive advantage over A. tonsa, that ensured their fast dispersal in the Black Sea, acclimatization in the new habitat and the successful competition over native species.

Analysis of potential changes in the Black Sea wave power for the 21st century

2021 ◽  
Vol 169 ◽  
pp. 512-526
Author(s):  
Burak Aydoğan ◽  
Tahsin Görmüş ◽  
Berna Ayat ◽  
Tunay Çarpar
Keyword(s):  
Black Sea ◽  
21St Century ◽  
The Black Sea ◽  
Wave Power ◽  
Sea Wave

scholarly journals Long term trends in the sea surface temperature of the Black Sea

Ocean Science ◽  
2010 ◽  
Vol 6 (2) ◽  
pp. 491-501 ◽  
Author(s):  
G. I. Shapiro ◽  
D. L. Aleynik ◽  
L. D. Mee
Keyword(s):  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Black Sea ◽  
Sea Surface ◽  
The Black Sea ◽  
The North ◽  
Sst Variability ◽  
Long Term Trends ◽  
Cooling Trend

Abstract. There is growing understanding that recent deterioration of the Black Sea ecosystem was partly due to changes in the marine physical environment. This study uses high resolution 0.25° climatology to analyze sea surface temperature variability over the 20th century in two contrasting regions of the sea. Results show that the deep Black Sea was cooling during the first three quarters of the century and was warming in the last 15–20 years; on aggregate there was a statistically significant cooling trend. The SST variability over the Western shelf was more volatile and it does not show statistically significant trends. The cooling of the deep Black Sea is at variance with the general trend in the North Atlantic and may be related to the decrease of westerly winds over the Black Sea, and a greater influence of the Siberian anticyclone. The timing of the changeover from cooling to warming coincides with the regime shift in the Black Sea ecosystem.

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