Reconstruction of radiation fluxes at the ocean surface from NOAA satellite data

Timofeev, N. A.; Ivanchik, M. V.; Sevostyanov, Andrey; Kikhai, Yu. V.

doi:10.1007/bf02197207

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“…In [2,[6][7][8]13], we describe and realize the algorithms of rapid evaluation of the quantities Q n and R n according to the data of scanning observations performed by using high-resolution radiometers in the spectral regions 0.725-1.1, 10.3-11.3, 8-12, and 3-30 μm. For the decadal and monthly values of Q n and R n , the errors have the same order of accuracy as for the shipborne observations, i.e., do not exceed 2-3%.…”

Section: World Ocean: Radiation Effective Cloudiness and Sea-surfacmentioning

confidence: 99%

“…For this purpose, one can use the monthly average values of F cn and SST for 1986-2002 from the PODAAC JRL AVHRR Pathfinder archive. The data (see E-mail: jorde@sea-store.jpl.gov and URL: http://podaac.jpl.nasa.gov/sst/) obtained from the NOAA- 7,9,14, and 16 satellites on a grid with space steps of 18 km [21] contains information on the intra-and interannual variations of the fields of LWOR, SST, and effective cloudiness on global and regional scales.…”

Section: Heat Exchange Of the Black Sea With The Atmospherementioning

confidence: 99%

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Climatic satellite monitoring of the external heat balance of the oceans and Black Sea

Timofeev

Yurovskii

2007

Phys Oceanogr

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The long-wave outgoing radiation, effective cloudiness equal to the product of the total cloud amount by their optical density, and the sea-surface temperature determined from the satellites are used to determine the annual course of the components of external heat balance on the sea surface whose climatic anomalies, parallel with the meridional heat and water transfer in the ocean-atmosphere system, specify the intraannual and interannual large-scale variations of weather in different regions of the Earth. The development of these studies is connected with the progress of satellite hydrophysics because the data obtained from the space become sufficiently exact, regular, and global. The increase in the existing data array on the external heat balance of the oceans from &15-20 to 100 yr and more would promote the solution of the problem of oscillations of Earth's climate. We present examples of coordinated numerical analysis of the heat balance of the upper (0-100 m ) layer of the Black Sea performed on the basis of the shipborne and satellite data.

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Section: World Ocean: Radiation Effective Cloudiness and Sea-surfacmentioning

confidence: 99%

Section: Heat Exchange Of the Black Sea With The Atmospherementioning

confidence: 99%

Climatic satellite monitoring of the external heat balance of the oceans and Black Sea

Timofeev

Yurovskii

2007

Phys Oceanogr

Self Cite

View full text Add to dashboard Cite

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Reconstruction of radiation fluxes at the ocean surface from NOAA satellite data

Cited by 1 publication

References 0 publications

Climatic satellite monitoring of the external heat balance of the oceans and Black Sea

Climatic satellite monitoring of the external heat balance of the oceans and Black Sea

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