Typical Distributions of Water Characteristics in the Oceans

Ocean Mean State Sea Surface Properties Vertical Structure Thermocline

Global Statistics Volumetric temperature-salinity diagram of the world ocean. 75% of the ocean's water have a temperature and salinity within the green region, 99% have a temperature and salinity within the region colored in cyan. The warm water outside the 75% region is confined to the upper 1000 m of the ocean. The mean temperature of the world ocean is 3.5 o C and the mean salinity is (Even at the equator the average temperature is as low as 4.9°C). 75% of the total volume of the ocean water has properties within the range from 0 o to 6 o C in temperature and 34 to 35 in salinity. 50% of the total volume of the oceans has properties between 1.3 o C and 3.8 o C and between 34.6 and Both temperature and salinity are quite uniformly distributed below 1000 m depth. From M. Tomczak, 1996: Introduction to Physical Oceanography (

Mean Sea Surface Temperature (SST) CPC Analysis, January 1982-December 2001 roughly zonal (east-west) isotherm meridional gradient follows solar radiation diverted north- south near the eastern coast (cold tongues) warm pool: SST > 28 o C sea ice at high latitudes (near -2 o C)

Mean Sea Surface Salinity (SSS) SSS distribution is mostly zonal (range: 33-37) Minimum north of the equator (ITCZ) Maximum in subtropics (trade winds) Lower around coast (river) and polar region (melting ice) Mediterranean, 39 and Red Sea, 41 (large evaporation ) NODC WOA98, levitus et al

SSS distribution in open ocean is closely linked to precipitation and sea surface evaporation From Pickard and Emery: Descriptive Physical Oceanography: An Introduction

Surface density (σ t ) σ t, 22 at equator, , 50 o -60 o latitude, decreases slightly further poleward σ t is affected by both the T and S distribution The temperature influence is more dominant

Temperature profiles In many ocean regions, temperature decreases with depth, results in an increase of density with depth and produces a stable density stratification. Vertically, there is an upper zone (mixed layer + thermocline) and a deep zone (with little change). Mixed layer: depth m. Temperature is close to SST. Permanent thermocline: depth m, temperature changes rapidly with depth. It is located at m depth in the tropics and at m depth in the subtropics and mid-latitudes. The temperature range is °C in mid- latitudes. (From Pickard and Emery: Descriptive Physical Oceanography: An Introduction)

At low and mid-latitudes, salinity decreases vertically and shows intermediate minima at 600 to 1000 m and then increases to 2000 m. They are linked with water mass formation at the Polar Fronts where precipitation is high. At very great depth, salinity increases again because the water near the ocean bottom originates from polar regions where it sinks during the winter; freezing during the process increases its salinity. A decrease in salinity produces a density decrease. Taken on its own, the salinity stratification would therefore produce an unstable density stratification. In the ocean the effect of the temperature decrease is stronger than the effect of the salinity decrease, so the ocean is stably stratified. Salinity Profiles Salinity increases at m in the tropics (sinking heavy waters and flowing equatorward) In high latitude: salinity increases with depth to 2000 m. (From Pickard and Emery: Descriptive Physical Oceanography: An Introduction)

subsurface density and pycnocline Density increases with depth (The gradient is not uniform) In the tropics, there is a shallow upper layer of nearly uniform density, then a layer where density increases rapidly (pycnocline), below this the density increases slowly in the deep zone. In deep water σ t =27.9 (with little change with latitude)

Mixed layer In a zone beneath the sea surface, properties are very well mixed vertically, particularly at the end of the night (diurnal cycle) and in winter (seasonal cycle). It is referred to as the mixed layer. The layer is mixed by wind (<150m) and surface cooling (can be as deep as 1000m). Re-stratified by surface warming, precipitation and adjacent mixed waters. Functional definition: depth at which the water is denser than the sigma-theta at the sea surface.

Kara, A. B., P. A. Rochford, and H. E. Hurlburt, 2003: Mixed layer depth variability over the global ocean. J. Geophys. Res., 108, doi: /2000C

Thermocline The region of higher vertical temperature gradient below the surface layer and above the abyssal layer is called the thermocline. In low and mid latitudes, a main or permanent thermocline exists all the time at depths between 200 and 1000 m. There is no permanent thermocline in polar and sub-polar waters (but usually a permanent “halocline” and associated “pycnocline” The thermocline water is given the water mass name “Central Water”

Ocean Stratification Potential density (σ θ ) as a function of latitude and depth in the Pacific Ocean. Note the scale difference between the depths about and below the upper 1000m. The density is quite uniformity below 1000 m depth in the range of

Temperature (top) and salinity (bottom) as functions of latitude and depth in the Pacific Ocean. (The image includes the Arctic Ocean on the extreme right.) Note the uniformity of both properties below 1000 m depth; the temperature is in the range 0 - 4°C, the salinity is near Temperature and Salinity Distributions

Enlarged T(top) and S(bottom) sections in the upper 1500 m of the Pacific Ocean. The highest temperature in the tropics is above 28°C. The permanent thermocline is the depth range of rapid temperature change, which in the tropics is found at m. Salinity also displays large changes in the upper 500 m, mainly in response to the precipitation - evaporation balance. In the depth range m the salinity is rather uniform at about 34.5 over most of the Pacific Ocean.

Equatorial Thermocline Note the high vertical temperature gradient around 20 o C isotherm.

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Mean 20 o C isotherm (unit: meter) The thermocline zone is sometimes characterized by the depth at which the temperature gradient is a maximum (the “thermocline depth”). In the equatorial ocean, 20 o C isotherm is a good indicator of the themocline location. The maxima of the 20 o C isotherm (the major warm waters in the upper ocean) are located differently from those of SST (The former is mainly determined by ocean dynamics while the latter by surface heat flux) Climatology from ocean data assimilation ( )