Isthmus of Tehuantepec Wind Climatology and ENSO Signal

@article{RomeroCenteno2003IsthmusOT,
  title={Isthmus of Tehuantepec Wind Climatology and ENSO Signal},
  author={Rosario Romero-Centeno and Jorge Zavala‐Hidalgo and Artemio Gallegos and James J. O'Brien},
  journal={Journal of Climate},
  year={2003},
  volume={16},
  pages={2628-2639}
}
Abstract The statistical characteristics of the winds at the Isthmus of Tehuantepec and their seasonal and interannual variability are studied through the analysis of several datasets and a reconstruction of the winds for a 31-yr period. Observations show that the long-term monthly mean wind speeds and frequency of occurrence of northerly winds have a strong seasonal signal, with maximum values during December–January, minimum during May–June, and a relative maximum in July. The frequency… 
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References

SHOWING 1-10 OF 25 REFERENCES
Noninertial flow in NSCAT observations of Tehuantepec winds
NASA scatterometer (NSCAT) observations provide high temporal and spatial resolution wind fields, which are used to examine gap flow through the Chivela Pass and the influence of Hurricane Marco. For
Supersquirt: Dynamics of the Gulf of Tehuantepec, Mexico
T H E LAST TWO DECADES have seen a continuing effort to observe and model the response to wind forcing in the coastal ocean along eastern boundaries of ocean basins. The emphasis of research has
Offshore wind forcing in the Gulf of Tehuantepec, Mexico: The asymmetric circulation
Since the early surveys carried out by the Eastern Tropical Pacific (EASTROPIC) and Scripps Tuna Oceanographic Research (STOR) projects in the tropical Pacific off Mexico, the northerly winds which
The midsummer drought over Mexico and Central America
Abstract The annual cycle of precipitation over the southern part of Mexico and Central America exhibits a bimodal distribution with maxima during June and September–October and a relative minimum
Inertial wind path and sea surface temperature patterns near the Gulf of Tehuantepec and Gulf of Papagayo
During the northern hemisphere winter the surface atmospheric pressure on the Gulf of Mexico side of Central America is often higher than that on the Pacific side. The resultant southward pressure
The Structure and Evolution of Gap Outflow over the Gulf of Tehuantepec, Mexico
Abstract Mesoscale-model simulations are used to examine the structure and dynamics of a gap-outflow event over the Gulf of Tehuantepec, Mexico, that was associated with a surge of cold air along the
Characteristics of wind‐generated rings in the eastern tropical Pacific Ocean
Eddies are generated in the eastern tropical Pacific (3°S–23°N, 75°–105°W) by winds blowing through Central American mountain passes from the Atlantic. We used Coastal Zone Color Scanner (CZCS) and
An Examination of the Frequency and Mean Conditions Surrounding Frontal Incursions into the Gulf of Mexico and Caribbean Sea
Abstract Maps of mean monthly frequency and duration of frontal incursions into the Gulf of Mexico and Caribbean Sea are presented for the 1965–72 period. The transition from the low-frequency regime
Satellite Observations of the Wind Jets off the Pacific Coast of Central America. Part II: Regional Relationships and Dynamical Considerations
Abstract Satellite estimates of winds at 10 m above the sea surface by the NASA scatterometer (NSCAT) during the 9-month period October 1996–June 1997 are analyzed to investigate the correlations
...
1
2
3
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