2 edition of On the space-time ocean current variability and its effects on the length-of-day. found in the catalog.
On the space-time ocean current variability and its effects on the length-of-day.
Nikolaos Theodoros Christou
by Dept. of Surveying Engineering, University of New Brunswick in Fredericton, N.B
Written in English
|Series||Technical report / Dept. of Surveying Engineering, University of New Brunswick -- no.148|
|Contributions||University of New Brunswick. Department of Surveying Engineering.|
|The Physical Object|
|Number of Pages||332|
waves contribution to length of day during ENSO in –, in IERS Technical Note The Impact of El Nino and Other Low-Frequency Signals on Earth Rotation and Global Earth System Parameters, edited by D. A. Salstein, B. Kolaczek, and D. Gambis. A global warming hiatus, also sometimes referred to as a global warming pause or a global warming slowdown, is a period of relatively little change in globally averaged surface temperatures. In the current episode of global warming many such year periods appear in the surface temperature record.
GGOS to meet its objectives, it must combine the greatest measurement precision (a relative precision of parts per billion =10 − 11) with utmost consistency in space, time, and applied data modeling, and with stability spanning decades. This is a key focus of GGOS. Godee ic t atOvions r e bs as a Fundato ion for essing As s and. "This is an interesting book to read now, but it promises to become an even more interesting book for future generations of physicists." Robert M. Wald, Science "Over the past thirty years, Stephen Hawking and Roger Penrose have done more than anyone to further our understanding of the nature of gravitation and cosmology/5(47).
North Paciﬁc. The two ocean basins are connected to each other only through their coupling to the common, zonally averaged atmosphere. The ocean–atmosphere coupling takes place via wind-driven torques and heat ﬂuxes at the air–sea interface. In this formulation, the decadal variability in each ocean basin consists of ocean–. These will have adverse effects on marine ecosystems 7. For example, in the west coast of Australia encountered sea surface temperatures that were 2–4 °C warmer than average for 10 by: 2.
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Winds, water density, and tides all drive ocean currents. Coastal and sea floor features influence their location, direction, and speed.
Earth’s rotation results in the Coriolis Effect which also influences ocean currents. Similar to a person trying to walk in a straight line across a spinning merry-go-round, winds and ocean waters get deflected from a straight line path as they travel. On Space-Time Ocean Current Variability and its Effects on the Length-of-Day (Issued as Technical Report ) ; OWOLABI, Karim: Simultaneous Distributional and Model Robustness in Bundle Adjustment: SANTERRE, Rock: Impact of GPS Satellite Sky Distribution (Issued as Technical Report ) SHIH, Peter Tian-Yuan.
Christou, N.T.:‘On the Space-Time Ocean Current Variability and its Effects on the Length-of-Day’, Ph.D. dissertation, Department of Surveying Engineering Technical Report No.University of New Brunswick, Fredericton, New Brunswick, Canada, pp.
Google ScholarCited by: Drought monitoring is crucial to water resource management and strategic planning. Thus, the objective of this study is to identify the space-time variability of hydrological drought across the broad arid region of northwestern China.
Seven distributions were applied to fitting monthly streamflow records of 16 gauging stations from 10 by: 1. Effects of El Niño Southern Oscillation on the space–time variability of Agricultural Reference Index for Drought in midlatitudes Article in Agricultural and Forest Meteorology Satellite ocean color images were used to determine the space-time variability of the Amazon River plume from – The relationship between sea-surface salinity (SSS) and the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) absorption coefficient for dissolved and detrital material (a dg) (r 2 =, n =30, rmse=) was used to identify the Amazon River plume low-salinity waters (Cited by: MERLE (Eds.) () Physical Oceanography of the Tropical Atlantic, GATE (prepared by V.
Lee), University of Miami, Miami, Florida. GARRETT C. and W. MUNK () Space-time scales of internal waves. Geophysical Research, 80, 3ournal GOULD W and E.
SAMBUCO () The effect of mooring type on measured values of ocean by: 7. Paleoceanography and Paleoclimatology publishes original research articles dealing with all aspects of understanding and reconstructing Earth’s past climate and environments from the Precambrian to modern analogs.
New lacustrine mineral‐magnetic records from Dahu Swamp in southern China provided a hydroclimatic reconstruction over the past. The importance of the diurnal variability of sea surface temperature (SST) on air-sea interaction is now being increasingly recognized.
This review synthesizes knowledge of the diurnal SST variation, mainly paying attention to its impact on the atmosphere or the ocean. Diurnal SST warming becomes evident when the surface wind is weak and insolation is by: the height of a point on the Earth's surface; the height above the Earth's surface.
in July, the thermal equator. trends poleward over continents and equatorward over the oceans. if there is a steeper pressure gradient, wind will be *blank than areas with a gradual pressure gradient. ISBN ). This book presents the results of curren fieldt remot, e sensing an, d modeling stud - ies of sea ice in different regions of the Southern Ocean and provide as n overview of the nature of Antarctic sea ice, its role in atmospheric and oceanographic pro-cesses, and its impact on the global environment.
This. where and are the estimates of the daily voluntary bear displacements in the u- and v-directions. The number of days, n, included in the time-series will affect our estimate of d.
For consistency, we set n to bethe length of the shortest time-series across the 15 by: When ocean and sea surfaces heat up sufficiently, evaporation occurs. The warm vapor rises into the atmosphere, then cools and condenses, releasing its stored latent heat.
Existing storms and tropical cyclones—which are called hurricanes in the Atlantic Ocean and typhoons in the Pacific and Indian oceans—gather up the released heat, which gives them greater energy and strength.
This book describes the principal dynamic processes that control the distribution of turbulence, its dissipation of kinetic energy and its effects on the dispersion of properties such as heat, salinity, and dissolved or suspended matter in the deep ocean, the shallow coastal and the continental shelf : S.
Thorpe. Tropical Indian Ocean is warming at a faster rate compared to other tropical oceans. The warming trends show a basin-scale surface warming with peak warming in the central equatorial Indian Ocean. This warming is favourable for weakening the monsoon Hadley circulation and strengthening the trade winds in the Pacific.
On the Space-time Ocean Current Variability and its Effects on the Length-of-Day Department of Surveying Engineering, Technical Report NoUniversity of Title: Independent Information.
One current theory of aging holds that, as the cells of a person's body start to hit this telomere-imposed limit, the lack of fresh, new cells causes the typical signs of aging: wrinkled skin, failing organs, weaker immune system, etc.
Whether or not telomere loss actually causes aging. In an earlier paper, Stammer and Wunsch (, hereinafter SW99) investigated temporal changes in the kinetic energy associated with variability over the global ocean using 4 yr of altimetric authors hypothesized 1) that parts of the observed variations in the flow field are caused by changes in direct wind forcing, especially in high latitudes, and 2) that an indirect nonlocal Cited by: By using a multi-river mixed-effects model we estimated the effects of oceanic and river conditions, as well as human impacts, on year-to-year and between-river variability across 60 time series of recreational catch of one-sea-winter salmon (grilse) from Norwegian rivers over 29 years (–).Cited by: 4.
Effects of Physical Processes on the Physiological Response of Individuals 5. Primary Production in Tidally Dominated Regimes 6. Conclusions References 1.
Introduction What we know of the ocean and, to a large extent, the questions we ask about it are the result of continual evolution of the observational tools available. In physical. Unfortunately, this book can't be printed from the OpenBook. If you need to print pages from this book, we recommend downloading it as a PDF.
Visit to get more information about this book, to buy it in print, or to download it as a free PDF. The Ocean is essential to life on Earth. Most of Earth's water is stored in the ocean.
Although 40 percent of Earth's population lives within, or near coastal regions- the ocean impacts people. a The global energy and water cycle (modified from Trenberth et al.
) and its alternative distributions: b in sea and land (modified from Hartmannwith values according to Trenberth et al. ) and c in latitude (modified from Hartmannwhich was based on Baumgartner and Reichel ; originally much older, at latest up to Meinardus’ analysis published in ; see Cited by: