Franklin Schwing | National Oceanographic Data Center (original) (raw)
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Papers by Franklin Schwing
Progress in Oceanography, 2011
Fisheries Oceanography, 2007
Eos, Transactions American Geophysical Union, 2004
Fisheries Oceanography, 2006
Oceanography, Dec 1, 2013
This report is a summary and preliminary analysis of recent observations of oceanographc and biol... more This report is a summary and preliminary analysis of recent observations of oceanographc and biological struc- ture of the California Current region, with emphasis on atmospheric pressure and wind fields, ocean circulation pattern and hydrographic structure, and upper-ocean plankton distributions. There was a strong transition in atmospheric circulation and sea-surface temperature be- tween the fall of 1994 and wintedspring 1995.
... NEWELL GARFIELD, DAN E. TRACY Department of Oceanography Naval Postgraduate School Monterey, ... more ... NEWELL GARFIELD, DAN E. TRACY Department of Oceanography Naval Postgraduate School Monterey, California 93943 ... Data Buoy Center (NDBC) moored buoys - 46013 (Bodega Bay: 38.2"N, 123.3"W); 46026 (Farallones: 37.8"N, 122.7"W); 46012 (Half Moon Bay: 37.4"N ...
Investigaciones Marinas, 2002
Geophys Res Lett, 2005
State-space models were applied to several climate indices associated with the El Niño-Southern O... more State-space models were applied to several climate indices associated with the El Niño-Southern Oscillation (ENSO), including the Southern Oscillation Index (SOI) and its component sea level pressure series; the NINO3 sea surface temperature index; and the Northern Oscillation Index (NOI). The best models for each series include a significant long-term nonparametric trend combined with a stochastic stationary cyclic term that clearly delineates the El Niño and La Niña events. There is no evidence that the frequency of ENSO events has changed over the 20th century. The long-term trend, however, has contributed to an apparent increase in the magnitude of recent El Niño events. This trend, potentially related to global warming, has increased the level of each series by an amount equal to 30-50% of the amplitude of their corresponding annual cycle or cyclic ENSO term. Thus, the background sea surface temperature in the eastern equatorial Pacific is more than 0.5°C warmer now than prior to 1950, implying a greater overall impact of El Niño events.
Progress in Oceanography, 2011
Fisheries Oceanography, 2007
Eos, Transactions American Geophysical Union, 2004
Fisheries Oceanography, 2006
Oceanography, Dec 1, 2013
This report is a summary and preliminary analysis of recent observations of oceanographc and biol... more This report is a summary and preliminary analysis of recent observations of oceanographc and biological struc- ture of the California Current region, with emphasis on atmospheric pressure and wind fields, ocean circulation pattern and hydrographic structure, and upper-ocean plankton distributions. There was a strong transition in atmospheric circulation and sea-surface temperature be- tween the fall of 1994 and wintedspring 1995.
... NEWELL GARFIELD, DAN E. TRACY Department of Oceanography Naval Postgraduate School Monterey, ... more ... NEWELL GARFIELD, DAN E. TRACY Department of Oceanography Naval Postgraduate School Monterey, California 93943 ... Data Buoy Center (NDBC) moored buoys - 46013 (Bodega Bay: 38.2"N, 123.3"W); 46026 (Farallones: 37.8"N, 122.7"W); 46012 (Half Moon Bay: 37.4"N ...
Investigaciones Marinas, 2002
Geophys Res Lett, 2005
State-space models were applied to several climate indices associated with the El Niño-Southern O... more State-space models were applied to several climate indices associated with the El Niño-Southern Oscillation (ENSO), including the Southern Oscillation Index (SOI) and its component sea level pressure series; the NINO3 sea surface temperature index; and the Northern Oscillation Index (NOI). The best models for each series include a significant long-term nonparametric trend combined with a stochastic stationary cyclic term that clearly delineates the El Niño and La Niña events. There is no evidence that the frequency of ENSO events has changed over the 20th century. The long-term trend, however, has contributed to an apparent increase in the magnitude of recent El Niño events. This trend, potentially related to global warming, has increased the level of each series by an amount equal to 30-50% of the amplitude of their corresponding annual cycle or cyclic ENSO term. Thus, the background sea surface temperature in the eastern equatorial Pacific is more than 0.5°C warmer now than prior to 1950, implying a greater overall impact of El Niño events.