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| Titel |
Marine boundary layer over the subtropical southeast Pacific during VOCALS-REx – Part 1: Mean structure and diurnal cycle |
| VerfasserIn |
D. A. Rahn, R. Garreaud |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1680-7316
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| Digitales Dokument |
URL |
| Erschienen |
In: Atmospheric Chemistry and Physics ; 10, no. 10 ; Nr. 10, no. 10 (2010-05-18), S.4491-4506 |
| Datensatznummer |
250008457
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| Publikation (Nr.) |
 copernicus.org/acp-10-4491-2010.pdf |
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| Zusammenfassung |
Atmospheric subsidence over the subtropical southeast Pacific (SEP) leads to
a low-level anticyclonic circulation, a cool sea surface and a cloud-topped
marine boundary layer (MBL). Observations in this region from a major field
campaign during October and November 2008, the VOCALS Regional Experiment,
provide ample data to characterize the lower atmospheric features over the
SEP. The observations are also useful to test the ability of an area-limited,
high-resolution atmospheric model to simulate the SEP conditions.
Observations and model-results (where appropriate) improve the
characterization of the mean state (Part 1) and variability (Part 2) of the
lower troposphere including circulation, MBL characteristics and the
upsidence wave.
Along 20° S the MBL is generally deeper offshore (1600 m at
85° W) but there is also considerable variability. MBL depth and
variability decrease towards the coast and maximum inversion strength is
detected between 74–76° W. Weather Research and Forecasting (WRF)
simulations underestimate MBL height the most near the coast but improve
offshore. Southeasterly trades prevail within the MBL although the wind speed
decreases toward the coast. Above the MBL along the coast of Chile, flow is
northerly, has a maximum at 3 km, and extends westward to
~74° W, apparently due to the mechanical blocking exerted by
the Andes upon the westerly flow aloft. Mean MBL features along northern
Chile (18–25° S) are remarkably similar (e.g., MBL depth just below
1 km) in spite of different SST. Observed diurnal cycles of the temperature
at the coast and further offshore exhibit a number of conspicuous features
that are consistent with the southwestward propagation of an upsidence wave
initiated during late evening along the south Peru coast. Furthermore, the
passage of the vertical motion results in either constructive or
deconstructive interference with the radiatively-forced diurnal cycle of MBL
depth. Interference is clearly seen in the soundings at Iquique which are
driven by a strong upsidence wave contrary to the radiation-driven cycle,
leading to a diurnal cycle opposite of the other sites. Because WRF
simulations have a lower MBL height, the speed of the simulated gravity wave
is slower than observations and accounts for most of the discrepancy between
observed and simulated phase speeds. |
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