Advantages of fine resolution SSTs for small ocean basins: Evaluation in the Black Sea

Download
2008-08-07
Kara, A. B.
Barron, C. N.
Wallcraft, A. J.
Oguz, T.
Casey, K. S.
This paper examines monthly variability of climatological mean sea surface temperature (SST) in the Black Sea. A total of eight products, including observation-and model-based SST climatologies, are formed and compared with each other. Some of the observation-based SST data sets include only satellite measurements, while others combine in situ temperatures, such as those from moored and drifter buoys, with satellite data. Climatologies for numerical weather prediction (NWP) model-based data sets are formed using high temporal resolution (6 hourly) surface temperatures. Spatial resolution of these SST products varies greatly (approximate to 4 km to 280 km), with the observation-based climatologies typically finer than the NWP-based climatologies. In the interior, all data sets are in general agreement, with annual mean SST biases typically within +/- 0.2 degrees C in comparison to the finest resolution (4 km) satellite-based Pathfinder climatology. Major differences are near the land-sea boundaries where model-based SSTs pose serious biases (as much as > 5 degrees C). Such errors are due to improper contamination of surface temperatures over land since coarse resolution model-based products cannot distinguish land and sea near the coastal boundaries. A creeping sea-fill interpolation improves accuracy of coastal SSTs from NWP climatologies, such as European Centre for Medium-Range Weather Forecast. All climatologies are also evaluated against historical in situ SSTs during 1942-2007. These comparisons confirm the relatively better accuracy of the observation-based climatologies.
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS

Suggestions

Simulation of annual plankton productivity cycle in the Black Sea by a one-dimensional physical-biological model
Oğuz, Temel; Ducklow, H; MalanotteRizzoli, P; Tuğrul, Süleyman; Nezlin, NP; Ünlüata, Ü (American Geophysical Union (AGU), 1996-07-15)
The annual cycle of the plankton dynamics in the central Black Sea is studied by a one-dimensional vertically resolved physical-biological upper ocean model, coupled with the Mellor-Yamada level 2.5 turbulence closure scheme. The biological model involves interactions between the inorganic nitrogen (nitrate, ammonium), phytoplankton and herbivorous zooplankton biomasses, and detritus. Given a knowledge of physical forcing, the model simulates main observed seasonal and vertical characteristic features, in p...
Tsunamis in the Black Sea: Comparison of the historical, instrumental, and numerical data
Yalçıner, Ahmet Cevdet; Talipova, T; Kurkin, A; Kozelkov, A; Zaitsev, A (American Geophysical Union (AGU), 2004-12-15)
The tsunami hazard in the Black Sea is discussed by comparing historical, instrumental data and numerical results. There are 22 tsunami events in the Black Sea documented since the first century, and nine of them have occurred in twentieth century. The numerical simulations of tsunami propagation for the 1966 and 1939 events are performed by using the framework of the shallow-water theory. The instrumental data from tide gauge records are used to compare and validate the simulation results and estimate the ...
Simulations of the Black Sea pelagic ecosystem by 1-D, vertically resolved, physical-biochemical models
Oguz, T; Ducklow, HW; Malanotte-Rizzoli, P; Murray, JW (Wiley, 1998-09-01)
The present paper summarizes the results of several simulations of the central Black Sea pelagic food web using three different 1-D, physical-biochemical, water column process models. The most simplified, five-compartment version is used to explore the robust biological features of the ecosystem and the role of upper-layer physics on the evolution of the euphotic zone biological processes. The other models, introducing additional biological complexities, show how these biologically structured models become ...
Density currents in the two-layer flow: an example of Dardanelles outflow
Besiktepe, ST (Elsevier BV, 2003-06-01)
Observations from hydrographic surveys are used to describe the density current flowing through the Dardanelles strait into the Marmara Sea. Aegean water plunges below the surface and flows into the Marmara Sea. This flow joins into the Marmara Sea as a negatively buoyant plume and sinks through the deeper parts. Seasonal variation in the incoming water density results in the observing mainly two different forms of the density current in this area. These two forms are boundary currents and intrusion. Bounda...
Modeling the response of top-down control exerted by gelatinous carnivores on the Black Sea pelagic food web
Oguz, T; Ducklow, HW; Purcell, JE; Malanotte-Rizzoli, P (American Geophysical Union (AGU), 2001-03-15)
Recent changes in structure and functioning of the interior Black Sea ecosystem are studied by a series of simulations using a one-dimensional, vertically resolved, coupled physical-biochemical model. The simulations are intended to provide a better understanding of how the pelagic food web structure responds to increasing grazing pressure by gelatinous carnivores (medusae Aurelia aurita and ctenophore Mnemiopsis leidyi) during the past 2 decades. The model is first shown to represent typical eutrophic ecos...
Citation Formats
A. B. Kara, C. N. Barron, A. J. Wallcraft, T. Oguz, and K. S. Casey, “Advantages of fine resolution SSTs for small ocean basins: Evaluation in the Black Sea,” JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, pp. 0–0, 2008, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/68103.