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A lot of text in 36 point This text is “justified” (both sides) The New Jersey coast, included...

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• A lot of text in 36 point •This text is “justified” (both sides) •The New Jersey coast, included in the Mid Atlantic Bight (MAB), is characterized by a broad shelf, where the 200 meter isobath (figure 1, in grey) is located approximately 70 and 100 Ezra Koenig 1 and Joe Strummer 2 [email protected], [email protected] 1 WHOI, Cape Cod, Kwassa Kwassa 2 Rutgers, the State University of New Jersey University, New Brunswick, NJ USA This is 96 point Futura Background (This is 48 point) Delaware Bay model phytoplankton Example Matlab plot: Conclusions Acknowledgements This work was made possible due to all the support and data provided by Rutgers Coastal Ocean Observation Lab and also due to IMAR/FLAD Tenore-Saldanha grant from the Luso-American Foundation. A big thanks to all who helped me with data treatment and to all that have contributed to the collection of all the data used. References: One place you can get away with a small font. This figure copied and pasted from the RUCOOL web site: 952 x 840 pixels (158kb) Charles Belmonte recommends you not use images that are smaller than about 100 kb and do not stretch small images like this or they will appear pixelated when printed poster size. • This is 20 point and is probably too small B A C Bigelow, H. B. (1933), Studies of the waters on the continental shelf, Cape Cod to Chesapeake Bay. I. The cycle of temperature, Pap. Phys. Oceanogr. Meteorol., 2, 135 pp. Bigelow, H. B., and M. Sears (1935), Studies of the waters on the continental shelf, Cape Cod to Chesapeake Bay. II. Salinity, Pap. Phys. Oceanogr. Meteorol., 4, 94 pp. Glenn, S., et al. (2004), Biogeochemical impact of summertime coastal upwelling on the New Jersey Shelf, J. Geophys. Res., 109, C12S02, doi:10.1029/2003JC002265. Glenn, S., Jones, C., Twardowski, M., Bowers, L., Kerfoot, J., Kohut, J., Webb, D., Schofield, O., 2008. Glider observations of sediment resuspension in a Middle Atlantic Bight fall transition storm. Limnol. Oceanogr., 53(5, part 2), 2008, 2180–2196 Kohut, J. T., S. M. Glenn, and R. J. Chant (2004), Seasonal current variability on the New Jersey inner shelf, J. Geophys. Res., 109, C07S07, doi:10.1029/2003JC001963. Moores, C. N. K., J. Fernandez-Partagas, and J. F. Price (1976), Meteoro- logical forcing fields of the New York Bight (first year’s progress report), Tech. Rep. TR76–8, Rosenstiel School of Mar. and Atmos. Sci., Univ. of Miami, Miami, Fla. •Storms forcing and water column stratification play an important role in defining the ocean structure. •Don’t make this too small • The highest values of backscatter were found near the bottom, between 29 th and 31 st of August and on the 4 th of September (figure 11A). ROMS: http://www.myroms.org S o S S o dz h h Equations from Mathtype: Use : format > color > Equations from Mathtype: Use : format > color > to change font color if you wish. to change font color if you wish. Text box 36 pt: The plot above is the actual size plotted from Matlab with: >> print –dpng –r300 filename The title text is Matlab 14pt Set the poster dimensions in: File > Page setup … to maximum of 48 inches by 36 inches from printing at IMCS
Transcript
Page 1: A lot of text in 36 point This text is “justified” (both sides) The New Jersey coast, included in the Mid Atlantic Bight (MAB), is characterized by a broad.

• A lot of text in 36 point

• This text is “justified” (both sides)

• The New Jersey coast, included in the Mid Atlantic Bight (MAB), is characterized by a broad shelf, where the 200 meter isobath (figure 1, in grey) is located approximately 70 and 100 …

Ezra Koenig1 and Joe Strummer2

[email protected], [email protected] WHOI, Cape Cod, Kwassa Kwassa 2 Rutgers, the State University of New Jersey University, New Brunswick, NJ USA

This is 96 point Futura

Background (This is 48 point) Delaware Bay model phytoplankton

Example Matlab plot:

Conclusions

AcknowledgementsThis work was made possible due to all the support and data provided by Rutgers Coastal Ocean Observation Lab and also due to IMAR/FLAD Tenore-Saldanha grant from the Luso-American Foundation. A big thanks to all who helped me with data treatment and to all that have contributed to the collection of all the data used.

References: One place you can get away with a small font.

This figure copied and pasted from the RUCOOL web site: 952 x 840 pixels (158kb)

Charles Belmonte recommends you not use images that are smaller than about 100 kb and do not stretch small images like this or they will appear pixelated when printed poster size.

• This is 20 point and is probably too small

B

A

C

Bigelow, H. B. (1933), Studies of the waters on the continental shelf, Cape Cod to Chesapeake Bay. I. The cycle of temperature, Pap. Phys. Oceanogr. Meteorol., 2, 135 pp.

Bigelow, H. B., and M. Sears (1935), Studies of the waters on the continental shelf, Cape Cod to Chesapeake Bay. II. Salinity, Pap. Phys. Oceanogr. Meteorol., 4, 94 pp.

Glenn, S., et al. (2004), Biogeochemical impact of summertime coastal upwelling on the New Jersey Shelf, J. Geophys. Res., 109, C12S02, doi:10.1029/2003JC002265.

Glenn, S., Jones, C., Twardowski, M., Bowers, L., Kerfoot, J., Kohut, J., Webb, D., Schofield, O., 2008. Glider observations of sediment resuspension in a Middle Atlantic Bight fall transition storm. Limnol. Oceanogr., 53(5, part 2), 2008, 2180–2196

Kohut, J. T., S. M. Glenn, and R. J. Chant (2004), Seasonal current variability on the New Jersey inner shelf, J. Geophys. Res., 109, C07S07, doi:10.1029/2003JC001963.

Moores, C. N. K., J. Fernandez-Partagas, and J. F. Price (1976), Meteoro- logical forcing fields of the New York Bight (first year’s progress report), Tech. Rep. TR76–8, Rosenstiel School of Mar. and Atmos. Sci., Univ. of Miami, Miami, Fla.

•Storms forcing and water column stratification play an important role in defining the ocean structure.

•Don’t make this too small

• The highest values of

backscatter were found

near the bottom, between

29th and 31st of August and

on the 4th of September

(figure 11A).

ROMS: http://www.myroms.org

So −SSo

dz−h

η

Equations from Mathtype: Use : format > color > Equations from Mathtype: Use : format > color > to change font color if you wish. to change font color if you wish.

Text box 36 pt: The plot above is the actual size plotted from Matlab with:

>> print –dpng –r300 filename

The title text is Matlab 14pt

Set the poster dimensions in:

File > Page setup …to maximum of 48 inches by 36 inchesfrom printing at IMCS

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