********************************************* PALEOCLIMATE MODELING INTERCOMPARISON PROJECT ********************************************* Newsletter N. 1 ---------------- 15 February 1993 Dear Participant, The present newsletter describes the recommended boundary conditions to be used for: -A- the fixed SST 6kyr BP experiment -B- the control run We also provide you with a preliminary list of output fields that will be useful for the intercomparison (-C-). You will also find: - an Appendix in which insolation values are provided for you to check your insolation calculations. - an updated list of the PMIP participants. Please do check all your informations again. We would like to be able to send you a "final" list in the next newsletter. ************************** -A- THE 6kyr BP EXPERIMENT ************************** The boundary conditions recommended for PMIP are: *1* SSTs and sea-ice prescribed at their present day value, as in the ---------------- control run. *2* No change in the land-surface characteristics. ---------------------------- *3* Carry out a 10-year simulation with full seasonal cycle to account for ------------------------------ interannual variability. *4* Greenhouse Gases ---------------- #4.1# Measurements from ice cores give the following concentrations at 6kyr BP (D.Raynaud, personal communication, June 1992): CO2 - CH4 - N20 ..................................................... 280 ppm - 650 ppb - 280 ppb #4.2# For models including only CO2: .............................. In order to be sure that we all get the same change in radiative forcing, we recommend setting the CO2 concentration for 6kyr BP as follows: C(6kyr BP) = (280/345) * control run concentration = 0.81 * control run concentration 345 ppm is the recommended value for CO2 concentration of the simulated present-day climate 280 ppm is the value at 6kyr BP obtained from ice core measurements Using the above formula, we will all get the same radiative forcing according to the IPCC report (1990): DF = 6.3 * ln(C/Co) = -1.3 W/m2 #4.3# For models including CO2 + other trace gases: ............................................. In this case the problem is more complicated. We recommend that you set all your concentrations in order to get the same total ********** change in radiative forcing, that is -1.3W/m2. This value must *************************** include the effects of all the trace gases. The forcing by CH4, N2O and CFC being non negligible (e.g. table 2.6 of the IPCC Report 1990), to keep the same change in radiative forcing implies that EITHER you only reduce the CO2 concentration value and keep other trace gases unchanged (i.e. present-day value) OR you change the concentration values of all your trace gases, but the change in CO2 will then certainly be less than what we suggested above. As far as we know, the GISS AGCM is the only one to prescribe trace gases other than CO2. BUT,if some other groups are concerned, please do let us know and we'll give you a set of concentration values, in agreement with GISS. *5* Insolation ---------- Insolation is the most important change to be prescribed in the boundary conditions for the 6kyr BP experiment. We must use the exact same forcing. #5.1# The orbital parameters are given by Andre BERGER (JAS, 1978): ...................... - Eccentricity: 0.018682 - Obliquity: 24.105 degrees - Longitude of perihelion (w), relative to the moving vernal equinox minus 180 degrees, i.e. angle between autumnal equinox and perihelion: 0.87 degrees #5.2# The solar constant must be kept as in the control run. .................. #5.3# The problem of calendar ....................... .5.3.1. It is NECESSARY that we all use the same reference date ********* for the 6kyr BP experiment, if we want to compare "comparable" climates. We then recommend that you set the 21 of March at noon (e.g. 21.00) as the date of your ******************* vernal equinox for the 6kyr BP simulation (for 360 as well as for 365-day year). Indeed, defining a calendar at 6kyr BP is arbitrary. Nevertheless it becomes very critical when we want to compare 2 climatic periods. We then need to know how to phase the 6kyr BP insolation pattern with the insolation pattern for the present-day climate. This is not trivial because the time intervals between equinoxes and solstices varies with the orbital parameters. For example, the number of days between the winter solstice and the vernal equinox changes from 89 days nowadays to 93 days 6kyr BP (for a 365-day year). Fixing the present date for the vernal equinox or for the winter solstice, at 6 kyr BP, then leads to 2 calendars differing by 4 days around the vernal equinox. A drift of 4 days in the insolation pattern is important: it leads to differences in insolation of the order of magnitude of the changes induced by the change in orbital parameters! .5.3.2. We recommend that you all keep DAILY VALUES ************ for as many variables as possible. Indeed we are working on defining a way to perform time-averages for the analyses, in order to best account for the change in insolation pattern. This part is still under work and will be discussed in another newsletter. We are also interested in keeping the daily values for circulation diagnoses such as monsoon statistics and transient circulation. *6* Checking insolation changes --------------------------- Before you start your simulations, we strongly advise that you check your computed insolation values. Indeed, Andre BERGER has warned us about the various approximations used by the GCMs that may induce differences in insolation that are not negligible with respect to the Milankovitch forcing. We thus provide you with tables for 1) the present- day and 2) 6 kyr BP minus present-day (see Appendix). We think that differences LARGER THAN 10% between your calculations of *************** 6 kyr BP minus present-day and ours SHOULD BE CORRECTED because they may ******************* significantly alter the model-model comparisons. If your calculations differ that much from our tables, we recommend that you carefully check your insolation code and send us a mail message reporting on the differences you found. We can then help clear up the differences. ****************************** -B- THE CONTROL RUN (optional) ****************************** Although the minimum requirements for PMIP are that we all use the exact same CHANGE in FORCING, we recommend that you redo your control run (if you can or if you need to) using AMIP recommendations: *1* PMIP datasets will be used for SSTs and sea-ice. ----------------------------------------------- They have been prepared at PCMDI and were calculated by averaging the 10-year AMIP datasets (1979-1988). They are available from NGDC. *2* Solar constant = 1365 W/m2 -------------- *3* Orbital parameters (1950 AD): ----------------------------- - Eccentricity: 0.016724 - Obliquity: 23.446 degrees - Longitude of perihelion (w), relative to the moving vernal equinox minus 180 degrees, i.e. angle between autumnal equinox and perihelion: 102.04 degrees *4* CO2 concentration = 345 ppm ----------------- *5* Carry out a 10-year simulation with full seasonal cycle ------------------ ********************* -C- THE OUTPUT FIELDS ********************* Here follows a preliminary list of outputs fields that we think will be useful for model-model or/and model-data comparisons. This list is based on the recommended diagnostics for AMIP (see AMIP newsletter N. 1, Sept.91) and results from discussions with some of you. Before finalizing the list of standard outputs for PMIP, to be gathered at one location, we would appreciate your comments. We are thinking about sending later a newsletter focused on this point. LIST ---- FIELDS # UNITS # ############################################################### # # * GENERAL FIELDS * # # .................. # # # # - Grid description # # - Surface elevation # m # - Surface type and fraction # # # # # # ############################################################### # # * ENERGY BUDGETS * # W/m2 # .................. # # # # TOP OF THE ATMOSPHERE # # # # - Incoming short-wave^ # # - Reflected short-wave^ # # - Outgoing long-wave^ # # # # SURFACE FLUXES # # # # - Incident short-wave^ # # - Reflected short-wave^ # # - Net long-wave^ # # - Sensible heat^ # # - Latent heat^ # # # # ############################################################### # # * HYDROLOGICAL CYCLE * # # ...................... # # # # - Soil moisture # kg/m2 # - Snow mass # kg/m2 # - Liquid precipitation, both # # large-scale and convective^ # mm/day # - Snow precipitation, both # # large-scale and convective^ # mm/day # - Evaporation and sublimation^ # mm/day # - Runoff # mm/day # - Total precipitable water # kg/m2 # # # ############################################################### # # * SURFACE CIRCULATION * # # ....................... # # # # - Surface air temperature # Celsius # - Ground temperature # Celsius # - Sea-level pressure # hPa # - Surface winds # m/s # - Wind stress components^ # N/m2 # - Relative humidity # % # # # ############################################################### # # * TROPOSPHERIC CIRCULATION * # # ............................ # # # # - 500hPa geopotential height # m # # # AT 850hPa AND 200hPa # # # # - Temperature # Celsius # - Zonal and meridional winds # m/s # - Specific humidity # g/kg # - Streamfunction # m2/s # - Velocity potential # m2/s # - Geopotential height # m # # # ############################################################### # # * CLOUDS and RADIATION * # # ........................ # # # # - Total cloudiness # # - Clear-sky outgoing long-wave # W/m2 # radiation # W/m2 # - Top of the atmosphere clear-sky # # reflected short-wave radiation # W/m2 # - Surface net clear-sky short-wave # # radiation # W/m2 # - Surface net clear-sky long-wave # # radiation # W/m2 # - Cloud liquid water (if possible) # g/m2 # # # ############################################################### # # * MERIDIONAL-VERTICAL # # DISTRIBUTION OF ZONAL MEANS * # # ............................... # # # # - Zonal and meridonal winds+ # m/s # - Temperature+ # Celsius # - Specific humidity+ # g/kg # - Relative humidity+ # # - Cloudiness+ # % # - Meridional streamfunction+ # kg/s # # # ############################################################### ^ Accumulated + At the standard pressure levels 1000, 850, 700, 500, 400, 300, 250, 200, 150, 100, 70, 50, 30, 20, 10 hPa Sincerely yours, Sylvie JOUSSAUME (LMCE, France) & Karl TAYLOR (LLNL, USA) ********** REFERENCES ********** * IPCC Report or Climate Change, Cambridge University Press, 354 pp, 1990. * Berger A., "Long-term variations of daily insolation and Quaternary climatic changes", JAS, 35, 2362-2367, 1978. **** N.B. **** * Please note that, if you reply to our mail by doing "reply" instead of "mail paleo..." every PMIP participant will receive your response. .... This is one of the mysteries of the network! * If you want to communicate information to all of us, we will be happy to forward it for you. We are thinking of having a mailbox box here that will be used for this type of "mail-to-be shared". ... But we are not there yet. *************************************** APPENDIX: About Insolation Computations *************************************** In the following, we provide tables and information concerning insolation in order to help you check your insolation code. All the results we give have been obtained using : - the orbital parameters given above in the present newsletter - a solar constant value of 1365 W/m2 - a calendar based on the 21 of March at noon (21.00) for the date of the vernal equinox. All the values of insolation are given in W/m2. They are given at every 10 degree of latitude (no latitudinal band average is done!). All the computations follow the method proposed by Berger (JAS, 1978) and are based on an expansion accurate to order e**3 for the computation of the true longitude (lambda, angle defining the Earth position relative to the Vernal Equinox). 1 - DATES of EQUINOXES and SOLSTICES ===================================== Present orbit : ------------- - 365 day year : date of vernal equinox = 21.00 march date of summer solstice = 21.73 June date of automnal equinox = 23.30 Sept date of winter solstice = 22.05 Dec date of perihelion = 2.85 Jan date of aphelion = 4.35 Jul - 360 day year date of vernal equinox = 21.00 march date of summer solstice = 22.46 June date of automnal equinox = 24.74 Sept date of winter solstice = 23.26 Dec date of perihelion = 4.91 Jan date of aphelion = 4.91 Jul 6 kyr BP orbit : -------------- - 365 day year : date of vernal equinox = 21.00 march date of summer solstice = 22.45 June date of automnal equinox = 19.56 Sept date of winter solstice = 17.61 Dec date of perihelion = 20.42 Sept date of aphelion = 21.92 March - 360 day year date of vernal equinox = 21.00 march date of summer solstice = 23.17 June date of automnal equinox = 21.06 Sept date of winter solstice = 18.89 Dec date of perihelion = 21.90 Sept date of aphelion = 21.90 March 2 - INSOLATION ============== We give insolation values for : - monthly means, which depend on the length of the year and on the reference date used - "mid-month" values which are daily mean insolation values given for specific true longitude values 2.1 Monthly means ------------------ * TODAY, 365 day year, 21.00 march vernal equinox -------------------------------------------------- LAT JAN FEB MAR APR MAY JUN JUL AUG SEP OCT NOV DEC 90. .00 .00 16.69 226.23 428.89 518.14 478.16 316.18 78.00 .00 .00 .00 80. .00 .50 58.88 229.60 422.37 510.27 470.89 311.54 116.50 10.87 .00 .00 70. .90 33.69 130.22 269.56 407.73 486.89 449.66 324.37 182.88 65.93 6.30 .00 60. 40.79 99.47 199.95 320.61 423.31 473.71 449.70 362.23 246.58 135.19 57.36 26.96 50. 106.32 169.74 264.21 365.91 444.60 480.35 462.83 397.32 303.52 203.70 124.80 89.30 40. 177.08 237.91 320.71 401.78 458.73 482.52 470.22 423.65 351.54 267.46 194.75 159.64 30. 246.98 300.58 367.62 426.40 462.36 475.32 467.72 438.95 389.07 323.90 262.21 230.72 20. 312.37 355.26 403.46 438.71 454.24 457.13 453.93 442.15 414.90 371.05 323.99 298.46 10. 370.54 400.05 427.12 438.20 434.07 427.68 428.57 432.88 428.22 407.35 377.68 359.92 0. 419.41 433.45 437.87 424.80 402.22 387.51 392.10 411.28 428.62 431.65 421.40 412.83 -10. 457.41 454.42 435.39 398.91 359.59 337.71 345.54 377.98 416.07 443.17 453.75 455.49 -20. 483.47 462.35 419.75 361.34 307.55 279.91 290.39 334.01 390.96 441.61 473.83 486.69 -30. 497.12 457.13 391.43 313.29 247.92 216.25 228.65 280.86 354.07 427.05 481.26 505.91 -40. 498.65 439.17 351.32 256.36 183.04 149.47 162.86 220.41 306.54 400.06 476.35 513.42 -50. 489.55 409.59 300.70 192.61 116.05 83.43 96.55 155.11 249.89 361.73 460.39 510.91 -60. 474.04 370.62 241.20 124.69 51.89 24.98 35.60 88.41 185.96 313.84 436.76 503.60 -70. 471.00 327.91 174.97 56.98 4.71 .00 .34 27.26 117.10 259.78 417.97 517.18 -80. 492.67 308.85 105.78 6.81 .00 .00 .00 .17 47.56 214.03 431.43 542.01 -90. 500.27 313.10 64.32 .00 .00 .00 .00 .00 7.99 206.29 438.09 550.37 * 6 kyrBP minus present day difference, 365 day year, 21.00 march ref --------------------------------------------------------------------- LAT JAN FEB MAR APR MAY JUN JUL AUG SEP OCT NOV DEC 90. .00 .00 -.92 -6.82 4.84 27.06 34.52 11.41 -16.01 .00 .00 .00 80. .00 .09 -2.28 -6.73 4.77 26.65 34.00 11.60 -11.76 -5.56 .00 .00 70. .15 -.31 -5.40 -7.58 4.30 25.43 32.33 14.40 -6.75 -13.79 -4.01 .00 60. -1.66 -3.42 -8.57 -8.83 2.82 20.95 28.54 17.27 -2.09 -13.72 -11.83 -5.09 50. -4.79 -7.12 -11.53 -9.95 2.10 18.78 27.25 19.85 2.51 -11.47 -13.64 -8.30 40. -8.20 -10.88 -14.17 -10.82 1.51 17.03 26.07 21.92 6.97 -8.15 -13.64 -10.63 30. -11.59 -14.46 -16.39 -11.38 .96 15.23 24.57 23.37 11.19 -4.19 -12.54 -12.36 20. -14.77 -17.71 -18.12 -11.63 .44 13.25 22.62 24.15 15.05 .16 -10.60 -13.55 10. -17.61 -20.49 -19.30 -11.54 -.05 11.10 20.21 24.22 18.43 4.71 -8.00 -14.22 0. -20.02 -22.72 -19.91 -11.11 -.49 8.79 17.39 23.58 21.24 9.29 -4.87 -14.35 -10. -21.91 -24.33 -19.92 -10.35 -.89 6.40 14.22 22.24 23.39 13.76 -1.31 -13.95 -20. -23.24 -25.26 -19.32 -9.30 -1.22 4.00 10.81 20.25 24.82 17.99 2.58 -13.03 -30. -23.97 -25.50 -18.15 -7.98 -1.46 1.70 7.30 17.67 25.47 21.88 6.72 -11.59 -40. -24.12 -25.07 -16.44 -6.43 -1.61 -.36 3.88 14.59 25.33 25.36 11.12 -9.64 -50. -23.76 -24.03 -14.23 -4.73 -1.61 -1.94 .80 11.11 24.39 28.47 15.87 -7.13 -60. -23.10 -22.54 -11.62 -2.93 -1.37 -2.48 -1.36 7.39 22.65 31.43 21.53 -3.76 -70. -23.12 -21.06 -8.71 -1.18 -.26 .00 -.12 3.68 20.10 35.20 32.19 1.44 -80. -24.39 -21.65 -5.75 -.02 .00 .00 .00 .36 16.37 45.79 37.93 1.51 -90. -24.76 -22.08 -4.44 .00 .00 .00 .00 .00 12.55 52.14 38.52 1.53 * TODAY, 360 day year, 21.00 march ref -------------------------------------- LAT JAN FEB MAR APR MAY JUN JUL AUG SEP OCT NOV DEC 90. .00 .00 14.32 220.76 425.37 517.27 481.36 326.53 89.18 .00 .00 .00 80. .00 .40 56.42 225.12 418.91 509.41 474.04 321.60 124.96 13.23 .00 .00 70. .41 30.86 127.79 266.40 404.82 486.07 452.55 331.24 189.96 70.96 7.88 .00 60. 37.96 95.66 197.70 318.04 421.39 473.20 451.54 367.47 252.75 140.56 60.60 27.46 50. 102.97 165.80 262.23 363.84 443.20 480.01 464.18 401.38 308.73 208.81 128.34 89.92 40. 173.73 234.23 319.06 400.20 457.77 482.31 471.14 426.63 355.71 271.97 198.16 160.26 30. 243.92 297.40 366.36 425.32 461.81 475.22 468.27 440.88 392.11 327.58 265.21 231.27 20. 309.81 352.78 402.63 438.15 454.07 457.14 454.12 443.06 416.74 373.71 326.38 298.89 10. 368.67 398.41 426.75 438.14 434.25 427.79 428.44 432.80 428.83 408.87 379.29 360.21 0. 418.36 432.77 437.98 425.23 402.73 387.69 391.67 410.26 427.99 431.93 422.12 412.95 -10. 457.29 454.77 435.97 399.80 360.39 337.96 344.85 376.10 414.24 442.17 453.49 455.41 -20. 484.37 463.79 420.78 362.64 308.58 280.22 289.49 331.38 388.01 439.30 472.52 486.41 -30. 499.11 459.68 392.89 314.94 249.12 216.59 227.59 277.62 350.10 423.45 478.86 505.40 -40. 501.80 442.85 353.17 258.30 184.34 149.82 161.73 216.75 301.71 395.23 472.82 512.66 -50. 493.95 414.42 302.88 194.72 117.34 83.76 95.44 151.25 244.37 355.70 455.67 509.90 -60. 479.97 376.73 243.65 126.85 53.00 25.23 34.68 84.68 179.99 306.62 430.65 502.25 -70. 480.02 335.84 177.64 58.95 5.10 .00 .22 24.40 111.01 251.15 409.41 515.18 -80. 502.64 320.03 108.67 7.71 .00 .00 .00 .03 42.22 202.07 420.81 539.92 -90. 510.39 324.56 67.38 .00 .00 .00 .00 .00 5.16 191.75 427.30 548.25 * 6 kyrBP minus present day, 360 day year, 21.00 march ref ---------------------------------------------------------- LAT JAN FEB MAR APR MAY JUN JUL AUG SEP OCT NOV DEC 90. .00 .00 -.79 -6.79 4.32 26.52 34.77 13.19 -16.25 .00 .00 .00 80. .00 .08 -2.16 -6.73 4.26 26.11 34.24 13.15 -11.17 -6.32 .00 .00 70. .10 -.21 -5.30 -7.64 3.80 24.92 32.58 15.53 -5.87 -13.93 -4.68 .00 60. -1.74 -3.23 -8.49 -8.93 2.40 20.51 28.63 18.15 -1.15 -13.48 -12.18 -5.42 50. -4.84 -6.91 -11.49 -10.08 1.70 18.37 27.24 20.55 3.44 -11.01 -13.80 -8.64 40. -8.19 -10.67 -14.16 -10.98 1.13 16.65 25.99 22.45 7.86 -7.54 -13.62 -10.88 30. -11.49 -14.28 -16.42 -11.57 .60 14.87 24.43 23.74 11.99 -3.48 -12.32 -12.48 20. -14.58 -17.55 -18.18 -11.84 .12 12.93 22.44 24.35 15.73 .94 -10.21 -13.51 10. -17.34 -20.38 -19.40 -11.76 -.33 10.82 20.00 24.25 18.97 5.51 -7.44 -13.99 0. -19.66 -22.66 -20.04 -11.33 -.73 8.56 17.14 23.45 21.62 10.09 -4.15 -13.93 -10. -21.48 -24.32 -20.07 -10.58 -1.08 6.21 13.96 21.96 23.59 14.52 -.46 -13.34 -20. -22.73 -25.31 -19.50 -9.51 -1.36 3.86 10.55 19.84 24.82 18.66 3.54 -12.22 -30. -23.40 -25.61 -18.35 -8.18 -1.56 1.61 7.05 17.14 25.28 22.44 7.77 -10.60 -40. -23.49 -25.25 -16.64 -6.61 -1.65 -.40 3.64 13.98 24.94 25.77 12.22 -8.47 -50. -23.09 -24.28 -14.45 -4.88 -1.61 -1.94 .61 10.45 23.81 28.70 16.99 -5.77 -60. -22.36 -22.86 -11.84 -3.05 -1.35 -2.46 -1.48 6.73 21.87 31.40 22.63 -2.17 -70. -22.28 -21.52 -8.92 -1.25 -.26 .00 -.10 3.14 19.11 34.78 33.09 3.53 -80. -23.45 -22.25 -5.96 -.04 .00 .00 .00 .17 15.01 44.73 39.58 3.69 -90. -23.81 -22.67 -4.66 .00 .00 .00 .00 .00 10.33 51.83 40.19 3.75 2.2 "MID-MONTH" values ----------------------- "Mid-month" values are obtained as daily mean insolation values in W/m2 and are computed at fixed true longitudes with longitude increments of 30 degrees, starting from the vernal equinox(Berger, JAS,1978) ... i.e. around the 20th of each month. Using this definition, we have : longitude = 0 corresponds to the vernal equinox (VE) longitude = 90 corresponds to the summer solstice (SS) longitude = 180 corresponds to the autumnal equinox (AE) longitude = 270 corresponds to the winter solstice (WS) These tables of "mid-month"values: 1) allow direct comparisons of insolation at equinoxes and solstices 2) avoid any problem of calendar, either between 0 and 6 kyr BP or between 360-day or 365-day years * "mid-month" values for present day orbit : ------------------------------------------- values are given for true longitude = 0, 30, 60 ... 330 degrees, starting from the vernal equinox VE SS AE WS LAT 0 30 60 90 120 150 180 210 240 270 300 330 90. .00 268.91 458.99 525.78 455.75 265.65 .00 .00 .00 .00 .00 .00 80. 76.02 264.83 452.02 517.79 448.83 261.62 74.97 .00 .00 .00 .00 .00 70. 149.73 293.64 431.31 494.07 428.27 290.08 147.65 41.80 .00 .00 .00 42.30 60. 218.89 340.45 439.55 478.21 436.45 336.32 215.85 109.80 44.19 24.42 44.49 111.13 50. 281.40 382.01 456.55 483.38 453.33 377.38 277.50 179.68 110.29 86.05 111.05 181.85 40. 335.35 414.14 467.01 484.40 463.72 409.12 330.71 246.31 180.74 156.34 181.99 249.28 30. 379.12 434.91 467.23 476.18 463.93 429.64 373.87 306.72 249.84 227.71 251.57 310.42 20. 411.37 443.30 455.87 457.07 452.65 437.93 405.67 358.65 314.11 295.99 316.28 362.98 10. 431.12 438.87 432.66 426.80 429.61 433.56 425.15 400.35 370.94 358.19 373.50 405.18 0. 437.77 421.66 398.04 385.90 395.23 416.56 431.71 430.45 418.31 412.00 421.20 435.64 -10. 431.12 392.18 352.96 335.50 350.47 387.43 425.15 448.02 454.70 455.66 457.84 453.42 -20. 411.37 351.33 298.88 277.24 296.78 347.07 405.67 452.54 479.09 487.98 482.40 458.00 -30. 379.12 300.45 237.73 213.29 236.06 296.82 373.87 443.97 491.03 508.38 494.42 449.33 -40. 335.35 241.28 171.98 146.44 170.76 238.36 330.71 422.77 490.80 517.15 494.19 427.87 -50. 281.40 176.01 104.94 80.60 104.20 173.88 277.50 389.97 479.81 516.06 483.12 394.67 -60. 218.89 107.56 42.05 22.87 41.75 106.26 215.85 347.54 461.94 510.55 465.12 351.73 -70. 149.73 40.95 .00 .00 .00 40.45 147.65 299.76 453.28 527.48 456.41 303.37 -80. 76.02 .00 .00 .00 .00 .00 74.97 270.34 475.04 552.81 478.32 273.60 -90. .00 .00 .00 .00 .00 .00 .00 274.52 482.37 561.33 485.70 277.83 * "mid-month" values for the 6 kyr BP minus present day difference : ------------------------------------------------------------------- VE SS AE WS LAT 0 30 60 90 120 150 180 210 240 270 300 330 90. .00 .99 14.92 31.77 36.20 22.30 .00 .00 .00 .00 .00 .00 80. -3.31 .98 14.69 31.29 35.65 21.96 3.38 .00 .00 .00 .00 .00 70. -6.52 -2.12 14.02 29.85 34.02 20.93 6.66 -1.35 .00 .00 .00 -4.39 60. -9.54 -4.05 9.69 24.84 29.89 22.56 9.74 -.23 -3.86 -4.20 -5.64 -8.42 50. -12.26 -5.67 7.90 22.33 28.81 24.12 12.52 1.34 -4.91 -7.36 -9.53 -12.17 40. -14.61 -7.05 6.42 20.33 27.74 25.19 14.93 3.05 -5.34 -9.83 -13.01 -15.55 30. -16.52 -8.17 5.00 18.25 26.28 25.63 16.87 4.76 -5.37 -11.81 -16.06 -18.46 20. -17.92 -9.01 3.61 15.96 24.32 25.39 18.31 6.40 -5.10 -13.33 -18.60 -20.80 10. -18.78 -9.56 2.23 13.45 21.84 24.46 19.19 7.89 -4.56 -14.36 -20.55 -22.52 0. -19.07 -9.81 .89 10.75 18.89 22.84 19.48 9.19 -3.79 -14.89 -21.87 -23.55 -10. -18.78 -9.74 -.36 7.94 15.55 20.58 19.19 10.25 -2.81 -14.91 -22.52 -23.87 -20. -17.92 -9.35 -1.50 5.10 11.93 17.77 18.31 11.05 -1.66 -14.40 -22.47 -23.46 -30. -16.52 -8.66 -2.46 2.36 8.18 14.49 16.87 11.56 -.34 -13.39 -21.72 -22.34 -40. -14.61 -7.68 -3.17 -.10 4.47 10.86 14.93 11.79 1.13 -11.85 -20.29 -20.54 -50. -12.26 -6.43 -3.53 -2.00 1.08 7.04 12.52 11.76 2.80 -9.78 -18.20 -18.12 -60. -9.54 -4.91 -3.23 -2.68 -1.46 3.25 9.74 11.55 4.86 -6.93 -15.45 -15.14 -70. -6.52 -3.06 .00 .00 .00 -.03 6.66 11.42 9.46 -2.96 -10.64 -11.69 -80. -3.31 .00 .00 .00 .00 .00 3.38 13.39 9.91 -3.10 -11.15 -7.65 -90. .00 .00 .00 .00 .00 .00 .00 13.60 10.06 -3.15 -11.32 -7.77 We hope all this information will help you ! Please let us know if it is unclear or if you have any trouble! ******************** LIST OF PARTICIPANTS ******************** BARTLEIN Patrick Department of Geography University of Oregon Eugene, Oregon 97403-1251 USA Tel.: 1 (503) 346.4967 Fax.: 1 (503) 346.2067 email: bartlein@oregon.uoregon.edu BAUM Steve ARC Technologies 305 Arguello Drive College Station, Texas 77840 USA Tel.: ? Fax.: 1 (409) 846.6280 email: baum_arc@sphinx.tamu.edu skb3832@zeus.tamu.edu BERGER Andre Institut d'Astronomie et de Geophysique G. Lemaitre Universite Catholique de Louvain 2 Chemin du Cyclotron B-1348 Louvain-la-Neuve BELGIUM Tel.: (32) 10 47.3297 (or: 47.3303) Fax.: (32) 10 47.4722 email: berger@astr.ucl.ac.be BRACONNOT Pascale Laboratoire de Modelisation du Climat et de l´Environnement D.S.M. / Orme des Merisiers / Bat. 709 C.E. Saclay 91191 Gif-sur-Yvette cedex FRANCE Tel.: (33) 1 69.08.77.11 Fax.: (33) 1 69.08.77.16 email: pmipweb@lsce.ipsl.fr BROCCOLI Anthony J. NOAA / Geophysical Fluid Dynamics Laboratory Princeton University P.O. Box 308 Princeton, NJ 08542 USA Tel.: 1 (609) 452.6671 Fax.: 1 (609) 987.5063 email: ajb@gfdl.gov BUDD William F. Meteorology Department University of Melbourne Parkville, Victoria 3052 AUSTRALIA Tel.: (61) 3 344.6909 Fax.: (61) 3 347.2091 email: ? CHANDLER Mark Goddard Institute for Space Studies / NASA 2880 Broadway avenue New York, NY 10025 USA Tel.: 1 (212) ? Fax.: 1 (212) 678.5552 email: ? CROWLEY Tom ARC Technologies 305 Arguello Drive College Station, Texas 77840 USA Tel.: 1 (409) 846.1403 Fax.: 1 (409) 846.6280 email: tom_arc@triton.tamu.edu FICHEFET Thierry Institut d'Astronomie et de Geophysique G. Lemaitre Universite Catholique de Louvain 2 Chemin du Cyclotron B-1348 Louvain-la-Neuve BELGIUM Tel.: (32) 10 47.3297 (or: 47.3295) Fax.: (32) 10 47.4722 email: fichefet@astr.ucl.ac.be GATES Larry Lawrence Livermore National Laboratory P.O. Box 808 L-264 Livermore, CA 94550 USA Tel.: 1 (510) 422.7626 Fax.: 1 (510) 422.7675 email: gates@kuala.llnl.gov !!!! UNREACHABLE !!!!! ********************** GHIL Michael Department of Atmospheric Sciences 7127 MSB University of California Los Angeles, CA 90024-1565 USA Tel.: ? Fax.: ? email: ghil@tuolumne.atmos.ucla.edu GUIOT Joel Laboratoire de Botanique Historique et de Palynologie Boite 451 Faculte de Saint-Jerome 13397 Marseille FRANCE Tel.: (33) 91.28.80.11 Fax.: (33) 91.28.86.68 email: lbhp@frmrs11.bitnet HALL Nick Department of Meteorology University of Reading 2 Earley Gate Whiteknigts, P.O. Box 329 Reading RG6 2AU UNITED KINGDOM Tel.: ? Fax.: (44) 734 35.2604 email: swshalnm@swssner1.reading.ac.uk HARRISON Sandy P. 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Director, Center for Climatic Research 1225 West Dayton Street Madison, WI 53706 USA Tel.: 1 (608) 262.2839 Fax.: 1 (608) 262.5964 email: jkutzbach@vms2.macc.wisc.edu LAUTENSCHLAGER Michael Deutsches Klimarechenzentrum GmbH Abt. Modellbetreuung Bundesstrasse 55 D-2000 Hamburg 13 GERMANY Tel.: (49) 40 411.73.297 Fax.: (49) 40 411.73.298 email: lautenschlager@dkrz-hamburg.dbp.de LE TREUT Herve Laboratoire de Meteorologie Dynamique E.N.S. 24 rue Lhomond 75231 Paris cedex 05 FRANCE Tel.: (33) 1 44.32.22.37 Fax.: (33) 1 43.36.83.92 email: letreut@lmd.ens.fr LOUTRE Marie-Francoise Institut d'Astronomie et de Geophysique G. Lemaitre Universite Catholique de Louvain 2 Chemin du Cyclotron B-1348 Louvain-la-Neuve BELGIUM Tel.: (32) 10 47.3297 (or: 47.3299) Fax.: (32) 10 47.4722 email: loutre@astr.ucl.ac.be MANABE Suki NOAA / Geophysical Fluid Dynamics Laboratory Princeton University P.O. 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Fax.: ? email: warren_prell@brown.edu RAMSTEIN Gilles Laboratoire de Modelisation du Climat et de l´Environnement D.S.M. / Orme des Merisiers / Bat. 709 C.E. Saclay 91191 Gif-sur-Yvette cedex FRANCE Tel.: (33) 1 69.08.77.11 Fax.: (33) 1 69.08.77.16 email: pmipweb@lsce.ipsl.fr RIND David Goddard Institute for Space Studies / NASA 2880 Broadway avenue New York, NY 10025 USA Tel.: 1 (212) 678.5593 Fax.: 1 (212) 678.5552 email: ? RUDDIMAN William Department of Environmental Sciences Clark Hall University of Virginia Charlottesville, VA 22903 USA Tel.: 1 (804) 924.7964 Fax.: 1 (804) 982.2137 email: ? SCHLESINGER Michael Department of Atmospheric Sciences University of Illinois @ Urbana-Champaign 105 South Gregory Avenue Urbana, IL 61801 USA Tel.: 1 (217) 333.2192 Fax.: 1 (217) 244.4393 email: schlesin@crg50.atmos.uiuc.edu schlesin@uiatma.atmos.uiuc.edu SCHNEIDER Steve National Center for Atmospheric Research P.O. Box 3000 Boulder, CO 80307 USA Tel.: ? Fax.: 1 (303) 497.1137 email: ? 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