Convergence zone

Results: 317



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61confirmed once again the existence of a wide convergence zone in the southwest Atlantic Ocean (Boltovskoy 1966, 1970, References Boltovskoy, ELa zona de Convergencla SubtropicaliSubantártica en el Océano

confirmed once again the existence of a wide convergence zone in the southwest Atlantic Ocean (Boltovskoy 1966, 1970, References Boltovskoy, ELa zona de Convergencla SubtropicaliSubantártica en el Océano

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 06:03:50
623 EARLY WIND FORECASTING RESULTS FROM THE 1.5 KM AAAAAAA AWRF-ARW IN EXTREME SOUTHWESTERN CALIFORNIA Ivory J. Small* and Brandt Maxwell NOAA/NWS San Diego, CA

3 EARLY WIND FORECASTING RESULTS FROM THE 1.5 KM AAAAAAA AWRF-ARW IN EXTREME SOUTHWESTERN CALIFORNIA Ivory J. Small* and Brandt Maxwell NOAA/NWS San Diego, CA

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Source URL: ams.confex.com

Language: English - Date: 2014-10-14 12:35:04
63VOLUME 22 JOURNAL OF CLIMATE 1 JANUARY 2009

VOLUME 22 JOURNAL OF CLIMATE 1 JANUARY 2009

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Source URL: web.maths.unsw.edu.au

Language: English - Date: 2011-03-08 16:46:57
64Clim Dyn DOIs00382x ENSO and non‑ENSO induced charging and discharging of the equatorial Pacific Bruce T. Anderson · Renellys C. Perez 

Clim Dyn DOIs00382x ENSO and non‑ENSO induced charging and discharging of the equatorial Pacific Bruce T. Anderson · Renellys C. Perez 

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Source URL: www.aoml.noaa.gov

Language: English - Date: 2015-04-08 10:42:06
65Microsoft Word - EES_Taschetto_Revised.doc

Microsoft Word - EES_Taschetto_Revised.doc

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Source URL: web.science.unsw.edu.au

Language: English - Date: 2010-08-23 17:33:45
66Monash Weather and Climate Seminar Series Friday May 2nd, 3pm, room 345, building 28 Dynamical response of the South Asian monsoon trough to latent heating from stratiform and

Monash Weather and Climate Seminar Series Friday May 2nd, 3pm, room 345, building 28 Dynamical response of the South Asian monsoon trough to latent heating from stratiform and

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Source URL: monash.edu.au

Language: English - Date: 2014-04-27 23:58:39
67The Four Questions Q1: How will storm tracks change in the future ? Storm tracks: Major component of the general circulation

The Four Questions Q1: How will storm tracks change in the future ? Storm tracks: Major component of the general circulation

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Source URL: www.euclipse.eu

Language: English - Date: 2014-08-01 05:59:20
68/home/disk/pynchon/emaroon/papers/cogs_paper/cogs_paper_figures_revised/figure1_qflux_topog_rev.eps

/home/disk/pynchon/emaroon/papers/cogs_paper/cogs_paper_figures_revised/figure1_qflux_topog_rev.eps

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Source URL: www.atmos.washington.edu

Language: English - Date: 2015-01-30 15:12:33
69Clim. Past, 10, 2007–2052, 2014 www.clim-past.netdoi:cp © Author(sCC Attribution 3.0 License. The global monsoon across timescales: coherent variability

Clim. Past, 10, 2007–2052, 2014 www.clim-past.netdoi:cp © Author(sCC Attribution 3.0 License. The global monsoon across timescales: coherent variability

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Source URL: aos.wisc.edu

Language: English - Date: 2015-01-30 23:47:44
70A Science and Implementation Plan for EPIC: An Eastern Pacific Investigation of Climate Processes in the Coupled Ocean-Atmosphere System COVER Upper panel: Idealized cross section through the cold-tongue/ITCZ complex in

A Science and Implementation Plan for EPIC: An Eastern Pacific Investigation of Climate Processes in the Coupled Ocean-Atmosphere System COVER Upper panel: Idealized cross section through the cold-tongue/ITCZ complex in

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Source URL: kestrel.nmt.edu

Language: English - Date: 2003-12-08 11:36:40