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| 6 |  |  | Circulation and Climate of the Ocean (ECCO) project homepage. ECCO is a consortium | 
| 7 |  |  | involving the Massachusetts Institute of Technology (MIT), the Jet Propulsion | 
| 8 |  |  | Laboratory (JPL/NASA), the Scripps Institution of Oceanography (SIO/SDSC) and the Institut | 
| 9 |  |  | fuer Meereskunde at the University of Hamburg (IfM). It is funded by the National | 
| 10 |  |  | Oceanographic Partnership Program (NOPP). The long term goal of ECCO is to provide | 
| 11 |  |  | a high resolution coupled ocean/sea-ice/biochemical (and ultimately, consistent | 
| 12 |  |  | atmospheric) state estimate to a wide community."> | 
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| 66 |  |  | <td height="22" valign="bottom" class="leftnavlink"> ecco report series </td> | 
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| 88 |  |  | <td width="563" height="1000" valign="top"><p class="headergray"><a href="posters.htm" class="textbox">back</a></p> | 
| 89 |  |  | <p class="headergray">JPL GROUP MEETING POSTERS</p> | 
| 90 |  |  | <p> Displayed here are our posters at various meetings. </p> | 
| 91 |  |  | <p> 2002: <a href="http://ecco.jpl.nasa.gov/external/posters.html#woce_2k2">WOCE</a> | <a href="#jason1_2k2a">Jason-1 (a)</a> | <a href="#igarss_2k2">IGARSS</a> | <a href="#godae_2k2">GODAE</a> | <a href="#jason1_2k2b">Jason-1 (b)</a> <br /> | 
| 92 |  |  | 2001: <a href="#agu_2k1">AGU 2001</a> | <a href="#jason1_2k1">Jason-1</a> | <a href="#woce_2k1">WOCE/JGOFS</a> | <a href="#nasa_2k1">NASA OSC</a> <br /> | 
| 93 |  |  | 2000: <a href="#tj_2k">TOPEX-JASON 2000</a> <br /> | 
| 94 |  |  | </p> | 
| 95 |  |  | <p> Please click on each image for larger plot in ps or pdf format. </p> | 
| 96 |  |  | <table border="0" cellpadding="5" cellspacing="0" class="border"> | 
| 97 |  |  | <tbody> | 
| 98 |  |  | <tr> | 
| 99 |  |  | <td colspan="3" bgcolor="#F1F4F8"><a name="woce_2k2">WOCE 2002<img src="images/spacer.gif" width="10" height="10" /></a></td> | 
| 100 |  |  | </tr> | 
| 101 |  |  | <tr> | 
| 102 |  |  | <td colspan="3"></td> | 
| 103 |  |  | </tr> | 
| 104 |  |  | <!-- one poster --> | 
| 105 |  |  | <tr> | 
| 106 |  |  | <td width="318" valign="top"> Seasonal-to-Interannual Variability of the Ocean During WOCE,  Estimated by the ECCO Routine Global Ocean Data Assimilation System <br /> | 
| 107 |  |  | WOCE and Beyond<br /> | 
| 108 |  |  | San Antonio, Texas<br /> | 
| 109 |  |  | November 18-22, 2002<br /> | 
| 110 |  |  | <br /> | 
| 111 |  |  | Overview of ECCO near real-time data assimilation system and examples  of its applications.  The system consists of a hierarchy of  assimilation methods that assimilate satellite sea surface height and  in situ temperature profiles.  Anayses are sensible and provide a  means to study ocean circulation.  Results are also used in geodetic  studies. </td> | 
| 112 |  |  | <td width="211"><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 113 |  |  | <tr> | 
| 114 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="pdfs/woce_posters/woce_ecco2.pdf" target="_blank"><img src="pdfs/pdf_images/woce_ecco2.jpg" width="166" height="128" border="0" class="img" /></a></div></td> | 
| 115 |  |  | </tr> | 
| 116 |  |  | </table></td> | 
| 117 |  |  | <td width="2"></td> | 
| 118 |  |  | </tr> | 
| 119 |  |  | <tr> | 
| 120 |  |  | <td colspan="3" bgcolor="#F3F2ED">  | 
| 121 |  |  | <!-- rm'ed <HR WIDTH=100% SIZE=1 noshade> --> | 
| 122 |  |  | <img src="images/spacer.gif" width="10" height="10" /></td> | 
| 123 |  |  | </tr> | 
| 124 |  |  | <!-- one poster --> | 
| 125 |  |  | <tr> | 
| 126 |  |  | <td valign="top"> An Open-Circuit and a Short-Circuit in the Pacific Ocean  Subtropical-Tropical Exchange <br /> | 
| 127 |  |  | WOCE and Beyond<br /> | 
| 128 |  |  | San Antonio, Texas<br /> | 
| 129 |  |  | November 18-22, 2002<br /> | 
| 130 |  |  | <br /> | 
| 131 |  |  | Pathway of subtropical-tropical exchange in the Pacific Ocean is  analyzed using a simulated passive tracer and its adjoint.  Intra-seasonal variability short-circuits the meridional exchange.  Contrary to the so-called "Subtropical Cell", the pathway of the  exchange is an open circuit and does not close. </td> | 
| 132 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 133 |  |  | <tr> | 
| 134 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="pdfs/woce_posters/woce_tracer_new.pdf" target="_blank"><img src="pdfs/pdf_images/woce_tracer_new.jpg" width="166" height="128" border="0" class="img" /></a></div></td> | 
| 135 |  |  | </tr> | 
| 136 |  |  | </table></td> | 
| 137 |  |  | <td></td> | 
| 138 |  |  | </tr> | 
| 139 |  |  | <tr> | 
| 140 |  |  | <td colspan="3" bgcolor="#F3F2ED">  | 
| 141 |  |  | <!-- rm'ed <HR WIDTH=100% SIZE=1 noshade> --> | 
| 142 |  |  | <img src="images/spacer.gif" width="10" height="10" /></td> | 
| 143 |  |  | </tr> | 
| 144 |  |  | <!-- one poster --> | 
| 145 |  |  | <tr> | 
| 146 |  |  | <td valign="top"> Interannual variation of mixed-layer heat balance: contrasting  different climate phenomena and the roles  of linear vs. nonlinear effects <br /> | 
| 147 |  |  | WOCE and Beyond<br /> | 
| 148 |  |  | San Antonio, Texas<br /> | 
| 149 |  |  | November 18-22, 2002<br /> | 
| 150 |  |  | <br /> | 
| 151 |  |  | Interannual variation of mixed-layer heat budget associated with the  climate events of El Nino, IOD, and PDO  phase switch during the period of 1997-2000 are examined using ECCO  assimilation product.  Similarity and  difference in interannual mixed-layer heat balance for these events are  discussed.  The role of nonlinear vs.  linear advective tendencies are addressed. </td> | 
| 152 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 153 |  |  | <tr> | 
| 154 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="pdfs/woce_posters/MLheat.pdf" target="_blank"><img src="pdfs/pdf_images/MLheat.jpg" width="166" height="128" border="0" class="img" /></a></div></td> | 
| 155 |  |  | </tr> | 
| 156 |  |  | </table></td> | 
| 157 |  |  | <td></td> | 
| 158 |  |  | </tr> | 
| 159 |  |  | <tr> | 
| 160 |  |  | <td colspan="3"></td> | 
| 161 |  |  | </tr> | 
| 162 |  |  | <tr> | 
| 163 |  |  | <td colspan="3" bgcolor="#F3F2ED"><img src="images/spacer.gif" width="10" height="10" /></td> | 
| 164 |  |  | </tr> | 
| 165 |  |  | <tr> | 
| 166 |  |  | <td colspan="3" bgcolor="#F1F4F8"><a name="jason1_2k2a">Jason-1 2002</a></td> | 
| 167 |  |  | </tr> | 
| 168 |  |  | <tr> | 
| 169 |  |  | <td colspan="3"></td> | 
| 170 |  |  | </tr> | 
| 171 |  |  | <!-- one poster --> | 
| 172 |  |  | <tr> | 
| 173 |  |  | <td valign="top"> Interannual Variation of Mixed-Layer Heat Balance <br /> | 
| 174 |  |  | Jason-1 Science Working Team Meeting<br /> | 
| 175 |  |  | New Orleans, Louisiana<br /> | 
| 176 |  |  | October 21-23, 2002<br /> | 
| 177 |  |  | <br /> | 
| 178 |  |  | The mixed-layer heat balance in key regions associated with events of  El Nino, Indian Ocean Dipole, and the Pacific Decadal Oscillation are  analyzed.  Advection plays a similar role in the study regions.  Differences in surface heat flux and diffusion is noted.  Nonlinear  advective tendencies are particularly important in El Nino. </td> | 
| 179 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 180 |  |  | <tr> | 
| 181 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="pdfs/jpl_posters/jason_021021.pdf" target="_blank"><img src="pdfs/pdf_images/jason_021021.jpg" width="166" height="128" border="0" class="img" /></a></div></td> | 
| 182 |  |  | </tr> | 
| 183 |  |  | </table></td> | 
| 184 |  |  | <td></td> | 
| 185 |  |  | </tr> | 
| 186 |  |  | <tr> | 
| 187 |  |  | <td colspan="3"></td> | 
| 188 |  |  | </tr> | 
| 189 |  |  | <tr> | 
| 190 |  |  | <td colspan="3" bgcolor="#F3F2ED"><img src="images/spacer.gif" width="10" height="10" /></td> | 
| 191 |  |  | </tr> | 
| 192 |  |  | <tr> | 
| 193 |  |  | <td colspan="3" bgcolor="#F1F4F8"><a name="igarss_2k2">IGARSS 2002</a></td> | 
| 194 |  |  | </tr> | 
| 195 |  |  | <tr> | 
| 196 |  |  | <td colspan="3"></td> | 
| 197 |  |  | </tr> | 
| 198 |  |  | <!-- one poster --> | 
| 199 |  |  | <tr> | 
| 200 |  |  | <td valign="top"> Mapping and Pseudo-Inverse Algorithms for Data Assimilation <br /> | 
| 201 |  |  | International Geoscience & Remote Sensing Symposium<br /> | 
| 202 |  |  | Toronto, Canada<br /> | 
| 203 |  |  | June 24-28, 2002<br /> | 
| 204 |  |  | <br /> | 
| 205 |  |  | Summary: Reduced-state Kalman filters require interpolation operators from the  reduced state to the fine grid and pseudo-inverse operators that map the fine  grid back to the reduced state.  This poster investigates a variety of  approaches to computing the pseudoinverse and evaluates the mapping  performance of eleven interpolation kernels. </td> | 
| 206 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 207 |  |  | <tr> | 
| 208 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="pdfs/jpl_posters/tmp.pdf" target="_blank"><img src="pdfs/pdf_images/tmp.jpg" width="166" height="215" border="0" class="img" /></a></div></td> | 
| 209 |  |  | </tr> | 
| 210 |  |  | </table></td> | 
| 211 |  |  | <td></td> | 
| 212 |  |  | </tr> | 
| 213 |  |  | <tr> | 
| 214 |  |  | <td colspan="3"></td> | 
| 215 |  |  | </tr> | 
| 216 |  |  | <tr> | 
| 217 |  |  | <td colspan="3" bgcolor="#F3F2ED"><img src="images/spacer.gif" width="10" height="10" /></td> | 
| 218 |  |  | </tr> | 
| 219 |  |  | <tr> | 
| 220 |  |  | <td colspan="3" bgcolor="#F1F4F8"><a name="godae_2k2">GODAE 2002</a></td> | 
| 221 |  |  | </tr> | 
| 222 |  |  | <tr> | 
| 223 |  |  | <td colspan="3"></td> | 
| 224 |  |  | </tr> | 
| 225 |  |  | <!-- one poster --> | 
| 226 |  |  | <tr> | 
| 227 |  |  | <td valign="top"> A Prototype GODAE Routine Global Ocean Data  Assimilation System: ECCO-2 <br /> | 
| 228 |  |  | International Symposium "En Route to GODAE"<br /> | 
| 229 |  |  | Biarritz, France<br /> | 
| 230 |  |  | June 13-15, 2002<br /> | 
| 231 |  |  | <br /> | 
| 232 |  |  | Summary: An overview of ECCO-2, a prototype routine global ocean data  assimilation system of ECCO.  The modeling and assimilation system are  introduced and some of their applications are described. </td> | 
| 233 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 234 |  |  | <tr> | 
| 235 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="pdfs/jpl_posters/ecco2.pdf" target="_blank"><img src="pdfs/pdf_images/ecco2.jpg" width="166" height="117" border="0" class="img" /></a></div></td> | 
| 236 |  |  | </tr> | 
| 237 |  |  | </table></td> | 
| 238 |  |  | <td></td> | 
| 239 |  |  | </tr> | 
| 240 |  |  | <tr> | 
| 241 |  |  | <td colspan="3" bgcolor="#F3F2ED">  | 
| 242 |  |  | <!-- rm'ed <HR WIDTH=100% SIZE=1 noshade> --> | 
| 243 |  |  | <img src="images/spacer.gif" width="10" height="10" /></td> | 
| 244 |  |  | </tr> | 
| 245 |  |  | <!-- one poster --> | 
| 246 |  |  | <tr> | 
| 247 |  |  | <td valign="top"> Physical Consistency of Data Assimilated Estimates and the ECCO  Hierarchical Assimilation Method <br /> | 
| 248 |  |  | International Symposium "En Route to GODAE"<br /> | 
| 249 |  |  | Biarritz, France<br /> | 
| 250 |  |  | June 13-15, 2002<br /> | 
| 251 |  |  | <br /> | 
| 252 |  |  | Summary: Temporal evolution of data assimilated solutions are  physically inconsistent (e.g., non-closed energy budgets) when  corresponding model errors are not determined.  The nature of the  inconsistency is described and its solution discussed. </td> | 
| 253 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 254 |  |  | <tr> | 
| 255 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="pdfs/jpl_posters/consistency.pdf" target="_blank"><img src="pdfs/pdf_images/consistency.jpg" width="166" height="117" border="0" class="img" /></a></div></td> | 
| 256 |  |  | </tr> | 
| 257 |  |  | </table></td> | 
| 258 |  |  | <td></td> | 
| 259 |  |  | </tr> | 
| 260 |  |  | <tr> | 
| 261 |  |  | <td colspan="3" bgcolor="#F3F2ED">  | 
| 262 |  |  | <!-- rm'ed <HR WIDTH=100% SIZE=1 noshade> --> | 
| 263 |  |  | <img src="images/spacer.gif" width="10" height="10" /></td> | 
| 264 |  |  | </tr> | 
| 265 |  |  | <!-- one poster --> | 
| 266 |  |  | <tr> | 
| 267 |  |  | <td valign="top"> Upper-ocean heat budget inferred from  ECCO-2 ocean data assimilation <br /> | 
| 268 |  |  | International Symposium "En Route to GODAE"<br /> | 
| 269 |  |  | Biarritz, France<br /> | 
| 270 |  |  | June 13-15, 2002<br /> | 
| 271 |  |  | <br /> | 
| 272 |  |  | Summary: The ECCO-2 ocean data assimilation product is used to examine anomalous  heat budget of the mixed layer  in several areas associated with different climate variations (ENSO,  Indian-Ocean Dipole, and PDO).  Similarities  and differences in heat budgets for the different climate variations are  highlighted. </td> | 
| 273 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 274 |  |  | <tr> | 
| 275 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="pdfs/jpl_posters/GODAE-02.pdf" target="_blank"><img src="pdfs/pdf_images/GODAE-02.jpg" width="166" height="128" border="0" class="img" /></a></div></td> | 
| 276 |  |  | </tr> | 
| 277 |  |  | </table></td> | 
| 278 |  |  | <td></td> | 
| 279 |  |  | </tr> | 
| 280 |  |  | <tr> | 
| 281 |  |  | <td colspan="3" bgcolor="#F3F2ED">  | 
| 282 |  |  | <!-- rm'ed <HR WIDTH=100% SIZE=1 noshade> --> | 
| 283 |  |  | <img src="images/spacer.gif" width="10" height="10" /></td> | 
| 284 |  |  | </tr> | 
| 285 |  |  | <!-- one poster --> | 
| 286 |  |  | <tr> | 
| 287 |  |  | <td valign="top"> Callibrating the ECCO Ocean General Circulation  Model Using Green's Functions <br /> | 
| 288 |  |  | International Symposium "En Route to GODAE"<br /> | 
| 289 |  |  | Biarritz, France<br /> | 
| 290 |  |  | June 13-15, 2002<br /> | 
| 291 |  |  | <br /> | 
| 292 |  |  | Summary: Green's functions provide a simple, yet effective, method to test and  calibrate General-Circulation-Model (GCM) parameterizations, to study and  quantify model and data errors, to correct model biases and trends, and to  blend estimates from different solutions and data products. </td> | 
| 293 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 294 |  |  | <tr> | 
| 295 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="pdfs/jpl_posters/poster.pdf" target="_blank"><img src="pdfs/pdf_images/poster.jpg" width="166" height="128" border="0" class="img" /></a></div></td> | 
| 296 |  |  | </tr> | 
| 297 |  |  | </table></td> | 
| 298 |  |  | <td></td> | 
| 299 |  |  | </tr> | 
| 300 |  |  | <tr> | 
| 301 |  |  | <td colspan="3"></td> | 
| 302 |  |  | </tr> | 
| 303 |  |  | <tr> | 
| 304 |  |  | <td colspan="3" bgcolor="#F3F2ED"><img src="images/spacer.gif" width="10" height="10" /></td> | 
| 305 |  |  | </tr> | 
| 306 |  |  | <tr> | 
| 307 |  |  | <td colspan="3" bgcolor="#F1F4F8"><a name="jason1_2k2b">Jason-1 2002</a></td> | 
| 308 |  |  | </tr> | 
| 309 |  |  | <tr> | 
| 310 |  |  | <td colspan="3"></td> | 
| 311 |  |  | </tr> | 
| 312 |  |  | <!-- one poster --> | 
| 313 |  |  | <tr> | 
| 314 |  |  | <td valign="top"> The Origin and Pathway of Nino3 Water Estimated  Using Products of the ECCO Data Assimilation System <br /> | 
| 315 |  |  | Jason-1 Science Working Team Meeting<br /> | 
| 316 |  |  | Biarritz, France<br /> | 
| 317 |  |  | June 10-12, 2002<br /> | 
| 318 |  |  | <br /> | 
| 319 |  |  | Summary: The origin and pathway of water occupying the surface layer  of the eastern Equatorial Pacific ("Nino3") are investigated using  passive tracers and their adjoint based on circulation estimates of  the ECCO Data Assimilation System ("ECCO-2"). </td> | 
| 320 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 321 |  |  | <tr> | 
| 322 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="pdfs/jpl_posters/tracer.pdf" target="_blank"><img src="pdfs/pdf_images/tracer.jpg" width="166" height="117" border="0" class="img" /></a></div></td> | 
| 323 |  |  | </tr> | 
| 324 |  |  | </table></td> | 
| 325 |  |  | <td></td> | 
| 326 |  |  | </tr> | 
| 327 |  |  | <tr> | 
| 328 |  |  | <td colspan="3" bgcolor="#F3F2ED">  | 
| 329 |  |  | <!-- rm'ed <HR WIDTH=100% SIZE=1 noshade> --> | 
| 330 |  |  | <img src="images/spacer.gif" width="10" height="10" /></td> | 
| 331 |  |  | </tr> | 
| 332 |  |  | <!-- one poster --> | 
| 333 |  |  | <tr> | 
| 334 |  |  | <td valign="top"> Interannual-to-decadal variation in tropical-subtropical  mass exchange in the Pacific Ocean boundary vs interior pathways <br /> | 
| 335 |  |  | Jason-1 Science Working Team Meeting<br /> | 
| 336 |  |  | Biarritz, France<br /> | 
| 337 |  |  | June 10-12, 2002<br /> | 
| 338 |  |  | <br /> | 
| 339 |  |  | Summary: Interannual-to-decadal variation of  tropical-subtropical mass exchange  in the Pacific Ocean is investigated  using sea level data, model simulation and assimilation.  Anomaly of boundary pycnocline transport is found  to be anti-correlated to and smaller in magnitude than that of the  interior, which are different from the  time-mean exchange. Forcing mechanisms are proposed to explain the  variations. </td> | 
| 340 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 341 |  |  | <tr> | 
| 342 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="pdfs/jpl_posters/JASON-02.pdf" target="_blank"><img src="pdfs/pdf_images/JASON-02.jpg" width="166" height="128" border="0" class="img" /></a></div></td> | 
| 343 |  |  | </tr> | 
| 344 |  |  | </table></td> | 
| 345 |  |  | <td></td> | 
| 346 |  |  | </tr> | 
| 347 |  |  | <tr> | 
| 348 |  |  | <td colspan="3"></td> | 
| 349 |  |  | </tr> | 
| 350 |  |  | <tr> | 
| 351 |  |  | <td colspan="3" bgcolor="#F3F2ED"><img src="images/spacer.gif" width="10" height="10" /></td> | 
| 352 |  |  | </tr> | 
| 353 |  |  | <tr> | 
| 354 |  |  | <td colspan="3" bgcolor="#F1F4F8"><a name="agu_2k1">AGU 2001</a></td> | 
| 355 |  |  | </tr> | 
| 356 |  |  | <tr> | 
| 357 |  |  | <td colspan="3"></td> | 
| 358 |  |  | </tr> | 
| 359 |  |  | <!-- one poster --> | 
| 360 |  |  | <tr> | 
| 361 |  |  | <td valign="top"> Application of an Ocean Model and its Adjoint for Global  Data Assimilation and Sensitivity Analysis <br /> | 
| 362 |  |  | AGU 2001 Fall Meeting<br /> | 
| 363 |  |  | San Francisco, California<br /> | 
| 364 |  |  | 10-14 December 2001<br />                    </td> | 
| 365 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 366 |  |  | <tr> | 
| 367 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="http://ecco.jpl.nasa.gov/external/posters/agufall2002.ps" target="_blank"><img src="pdfs/pdf_images/agufall2002.jpg" width="166" height="127" border="0" class="img" /></a></div></td> | 
| 368 |  |  | </tr> | 
| 369 |  |  | </table></td> | 
| 370 |  |  | <td></td> | 
| 371 |  |  | </tr> | 
| 372 |  |  | <tr> | 
| 373 |  |  | <td colspan="3"></td> | 
| 374 |  |  | </tr> | 
| 375 |  |  | <tr> | 
| 376 |  |  | <td colspan="3" bgcolor="#F3F2ED"><img src="images/spacer.gif" width="10" height="10" /></td> | 
| 377 |  |  | </tr> | 
| 378 |  |  | <tr> | 
| 379 |  |  | <td colspan="3" bgcolor="#F1F4F8"><a name="jason1_2k1">Jason-1 2001</a></td> | 
| 380 |  |  | </tr> | 
| 381 |  |  | <tr> | 
| 382 |  |  | <td colspan="3"></td> | 
| 383 |  |  | </tr> | 
| 384 |  |  | <!-- one poster --> | 
| 385 |  |  | <tr> | 
| 386 |  |  | <td valign="top"> The Three-Dimensional Circulation of the Ocean <br /> | 
| 387 |  |  | Jason-1 Science Working Team Meeting<br /> | 
| 388 |  |  | Solvang, California<br /> | 
| 389 |  |  | 6 December 2001<br /> | 
| 390 |  |  | <br /> | 
| 391 |  |  | Summary:  The poster is an introduction to our project and describes what data   assimilation is about and what its applications are.  Satellites provide   the most extensive observation of the ocean but are limited to measuring   properties of the sea surface.  Data assimilation combines these   observations with models and thereby extrapolates the measurements into   complete descriptions of the ocean.  Deep circulation is revealed and   processes underlying observed changes are identified.  Data assimilation   helps improve our understanding of ocean circulation.  These advancements   also help improve understandings of biogeochemical cycles and changes in   earth rotation. </td> | 
| 392 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 393 |  |  | <tr> | 
| 394 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="http://ecco.jpl.nasa.gov/external/posters/jason_011206.ps" target="_blank"><img src="pdfs/pdf_images/jason_011206.jpg" width="166" height="127" border="0" class="img" /></a></div></td> | 
| 395 |  |  | </tr> | 
| 396 |  |  | </table></td> | 
| 397 |  |  | <td></td> | 
| 398 |  |  | </tr> | 
| 399 |  |  | <tr> | 
| 400 |  |  | <td colspan="3"></td> | 
| 401 |  |  | </tr> | 
| 402 |  |  | <tr> | 
| 403 |  |  | <td colspan="3" bgcolor="#F3F2ED"><img src="images/spacer.gif" width="10" height="10" /></td> | 
| 404 |  |  | </tr> | 
| 405 |  |  | <tr> | 
| 406 |  |  | <td colspan="3" bgcolor="#F1F4F8"><a name="woce_2k1">WOCE/JGOFS 2001</a></td> | 
| 407 |  |  | </tr> | 
| 408 |  |  | <tr> | 
| 409 |  |  | <td colspan="3"></td> | 
| 410 |  |  | </tr> | 
| 411 |  |  | <!-- one poster --> | 
| 412 |  |  | <tr> | 
| 413 |  |  | <td valign="top"> Pacific and Indian Ocean Circulation During 1993-2000:  Assimilation of TOPEX/Poseidon Data into a Near Global OGCM <br /> | 
| 414 |  |  | WOCE/JGOFS Transport Workshop<br /> | 
| 415 |  |  | Southampton, UK<br /> | 
| 416 |  |  | 25-29 June 2001<br />                    </td> | 
| 417 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 418 |  |  | <tr> | 
| 419 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="http://ecco.jpl.nasa.gov/external/posters/woce_southampton_2001.ps" target="_blank"><img src="pdfs/pdf_images/woce_southampton_2001.jpg" width="166" height="127" border="0" class="img" /></a></div></td> | 
| 420 |  |  | </tr> | 
| 421 |  |  | </table></td> | 
| 422 |  |  | <td></td> | 
| 423 |  |  | </tr> | 
| 424 |  |  | <tr> | 
| 425 |  |  | <td colspan="3"></td> | 
| 426 |  |  | </tr> | 
| 427 |  |  | <tr> | 
| 428 |  |  | <td colspan="3" bgcolor="#F3F2ED"><img src="images/spacer.gif" width="10" height="10" /></td> | 
| 429 |  |  | </tr> | 
| 430 |  |  | <tr> | 
| 431 |  |  | <td colspan="3" bgcolor="#F1F4F8"><a name="nasa_2k1">NASA OSC 2001</a></td> | 
| 432 |  |  | </tr> | 
| 433 |  |  | <tr> | 
| 434 |  |  | <td colspan="3"></td> | 
| 435 |  |  | </tr> | 
| 436 |  |  | <!-- one poster --> | 
| 437 |  |  | <tr> | 
| 438 |  |  | <td valign="top"> Toward Operational Ocean State Estimation <br /> | 
| 439 |  |  | NASA Oceanography Scientific Conference<br /> | 
| 440 |  |  | Oceanology International Americas<br /> | 
| 441 |  |  | Miami Beach, Florida<br /> | 
| 442 |  |  | April 3-5, 2001<br />                    </td> | 
| 443 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 444 |  |  | <tr> | 
| 445 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="http://ecco.jpl.nasa.gov/external/posters/poster_nasa_miami2.ps" target="_blank"><img src="pdfs/pdf_images/poster_nasa_miami2.jpg" width="166" height="127" border="0" class="img" /></a></div></td> | 
| 446 |  |  | </tr> | 
| 447 |  |  | </table></td> | 
| 448 |  |  | <td></td> | 
| 449 |  |  | </tr> | 
| 450 |  |  | <tr> | 
| 451 |  |  | <td colspan="3" bgcolor="#F3F2ED">  | 
| 452 |  |  | <!-- rm'ed <HR WIDTH=100% SIZE=1 noshade> --> | 
| 453 |  |  | <img src="images/spacer.gif" width="10" height="10" /></td> | 
| 454 |  |  | </tr> | 
| 455 |  |  | <!-- one poster --> | 
| 456 |  |  | <tr> | 
| 457 |  |  | <td valign="top"> Tropical Pacific and Indian Ocean Heat Balance Inferred  by Assimilation TOPEX Dat into a Near-global OGCM <br /> | 
| 458 |  |  | NASA Oceanography Scientific Conference<br /> | 
| 459 |  |  | Oceanology International Americas<br /> | 
| 460 |  |  | Miami Beach, Florida<br /> | 
| 461 |  |  | April 3-5, 2001<br />                    </td> | 
| 462 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 463 |  |  | <tr> | 
| 464 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="http://ecco.jpl.nasa.gov/external/posters/poster_nasa_miami1.ps" target="_blank"><img src="pdfs/pdf_images/poster_nasa_miami1.jpg" width="166" height="128" border="0" class="img" /></a></div></td> | 
| 465 |  |  | </tr> | 
| 466 |  |  | </table></td> | 
| 467 |  |  | <td></td> | 
| 468 |  |  | </tr> | 
| 469 |  |  | <tr> | 
| 470 |  |  | <td colspan="2" valign="top" bgcolor="#F3F2ED"><img src="images/spacer.gif" width="10" height="10" /></td> | 
| 471 |  |  | <td></td> | 
| 472 |  |  | </tr> | 
| 473 |  |  | <tr> | 
| 474 |  |  | <td colspan="2" valign="top" bgcolor="#F1F4F8"><a name="tj_2k">TOPEX-JASON 2000</a></td> | 
| 475 |  |  | <td></td> | 
| 476 |  |  | </tr> | 
| 477 |  |  | <tr> | 
| 478 |  |  | <td valign="top">Interannual Variability of the Indonesian Throughflow  Transport Estimated from Wind Stress and Adjoint Sensitivity <br /> | 
| 479 |  |  | TOPEX-JASON SWT meeting<br /> | 
| 480 |  |  | Miami Beach, Florida<br /> | 
| 481 |  |  | 2000</td> | 
| 482 |  |  | <td><table border="0" align="right" cellpadding="0" cellspacing="0" class="img"> | 
| 483 |  |  | <tr> | 
| 484 |  |  | <td width="147" height="106" align="center"><div align="center"><a href="http://ecco.jpl.nasa.gov/external/posters/adj_sen.ps" target="_blank"><img src="pdfs/pdf_images/adj_sen.jpg" width="166" height="117" border="0" class="img" /></a></div></td> | 
| 485 |  |  | </tr> | 
| 486 |  |  | </table></td> | 
| 487 |  |  | <td></td> | 
| 488 |  |  | </tr> | 
| 489 |  |  | <tr> | 
| 490 |  |  | <td colspan="3"></td> | 
| 491 |  |  | </tr> | 
| 492 |  |  | <tr> | 
| 493 |  |  | <td colspan="3" bgcolor="#F3F2ED"><img src="images/spacer.gif" width="10" height="10" /></td> | 
| 494 |  |  | </tr> | 
| 495 |  |  |  | 
| 496 |  |  | <!-- one poster --> | 
| 497 |  |  | </tbody> | 
| 498 |  |  | </table> | 
| 499 |  |  | <p class="headergray"> </p> | 
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