but if a few organizations have a consensus, thats not the same as the whole scientific community having a consensusi mean just post a link to the overwhelming consensus pre-IPCC report if there are so many]
6/5/2007 4:50:12 PM
A "few?"Please.A consensus was widely acknowledged among the scientific community, and the IPCC report had no effect on it. The only reason it's cited so often is because it's the latest and greatest. [Edited on June 5, 2007 at 5:00 PM. Reason : .]
6/5/2007 4:57:50 PM
i mean just post a link to the overwhelming consensus pre-IPCC report if there are so many
6/5/2007 5:04:30 PM
I enjoy the questions due to Mr. aaronburro.
6/5/2007 5:15:04 PM
As mentioned before in this thread, the American Association for the Advancement of Science, the US National Academy of Science, the Joint Science Academies, and the American Meteorological Society all accepted a consensus before the report came out.Do you mean to tell me that that doesn't represent a consensus?
6/5/2007 5:15:50 PM
6/5/2007 5:16:09 PM
http://www.aaas.org/news/press_room/climate_change/mtg_200702/aaas_climate_statement.pdfNow...
6/5/2007 5:24:05 PM
6/5/2007 5:25:42 PM
http://dels.nas.edu/dels/rpt_briefs/climate-change-final.pdfhttp://www.ametsoc.org/POLICY/climatechangeresearch_2003.html
6/5/2007 5:28:01 PM
ok, the first link doesnt even mention a consensus...do you even read the links you're posting?and the 2nd link claims a consensus amongst the AMS, not the scientific communitylet alone your whole premise is trying to prove that a majority of people's opinion is that humans are fucking up the planet...now thats some exact data!
6/5/2007 5:35:45 PM
I'm trying to prove that among scientists, there's a consensus on anthropogenic climate change.I think that citing a number of major scientific organizations representing a significant number of scientists achieves that end. Meanwhile, you've given me nothing to counter these organizations.Or did you want to throw in those Canadians into the mix?Oh, and bullshit. The first one says, and I quote: "humans have had an impact on climate"[Edited on June 5, 2007 at 5:46 PM. Reason : .]
6/5/2007 5:43:29 PM
No thats not at all what you were trying to prove. You were trying to prove that there was a consensus among the scientific community of anthropogenic climate change before the IPCC report was releasedAnd what Canadians do you keep babbling about? Why don't you throw some NC State professors in the mix.
6/5/2007 6:57:35 PM
Dude,I've demonstrated that major scientific associations supported climate change before and after the IPCC report. You've yet to link to a single shred of evidence demonstrating otherwise.Until you do, you're just trolling.[Edited on June 5, 2007 at 8:40 PM. Reason : .]
6/5/2007 8:40:14 PM
sure thing van driesen
6/5/2007 8:59:34 PM
6/6/2007 12:18:11 AM
And W got the idea from those environment-hating, profit-driven Europeans!! .... A Cap-and-Trade policy for greenhouse gases have been in place in the EU for more than 2 years. It's a learning process for both businesses and policymakers. Try to keep up.here's a recent link:http://www.americanprogress.org/issues/2007/06/g8_cap_and_trade.html[Edited on June 6, 2007 at 12:30 AM. Reason : 2]
6/6/2007 12:28:08 AM
6/6/2007 12:32:11 AM
You're trying to say that the EU copied from W's proposal for the Clear Skies Act? Are you joking? The Europeans were hatching this idea before Bush even came into office. Here's a paper about Denmark's cap-and-trade program which was started in 1999.http://www.ghgprotocol.org/DocRoot/6FsOBJXLaLck3X9FToIp/Danish_CO2_cap_Final.pdf[Edited on June 6, 2007 at 12:44 AM. Reason : 2]
6/6/2007 12:40:55 AM
6/6/2007 1:37:43 AM
I never mentioned the EU. You did. I am saying that it's not just capitalism hating, sandal wearing, hippy environmentalists who are trying to advocate for cap and trade. But I guess W. gets a free pass, right?
6/6/2007 2:53:00 AM
"They call this a consensus?"
6/6/2007 4:05:29 AM
6/6/2007 5:00:33 AM
^1. Your post is bullshit--as usual.2. The title of the report follows (note that it is the short version):Questioning the Global Warming Science:An annotated bibliography of recent peer-reviewed papers(Short Version)3. The papers are all peer-reviewed and do not support the so-called consensus and the so-called science of global warming, which was the point. 4. Why didn't you post the entire list of summaries and conclusions? Talk about taking something out of context--no matter, I'll post them for you:Summary & Conclusions1. The recent warming of the earth’s surface (~0.4°C ) is significantly influenced by humanactivity on ground like urbanization, land-use change etc. The warming due solely to human-added CO2 appears to be a smaller part of the total recent warming.2. Solar variability and changes in large-scale atmospheric flow patterns in recent years havealso contributed to some of the recent warming of the earth’s surface.3. The Arctic basin temperature changes of the last 125 years, appear to be intimately linked tothe Total Soar Irradiance (TSI) while showing a weak correlation with atmospheric CO2concentrations.4. The earth’s climate experienced Rapid Climate Change during the entire Holocene period.and in particular during the last 5000 years or so. Ice core and other proxy data documentmid-Holocene warming of the Arctic as well as the Antarctic. This Holocene warmingappears to be strongly linked to solar variability and not to the greenhouse gas forcing.5. There does not appear any discernible link between Global Warming and recent increase inextreme weather events world-wide. The apparent increase in extreme weather events ismore a perception than reality, this perception being created due to increased mediaattention and publicity of extreme weather events.6. North Atlantic hurricanes appear to have strengthened in recent years; however typhoonsand tropical cyclones in other ocean basins do not show consistent increase in strength inrecent years.7. The Sea Level Rise of the 20th century is influenced significantly by inter-decadal variability.The most recent study (published January 2007) shows that the sea-level change in the lastfifty years were smaller than those in the early part of the 20th century. There is no evidenceof accelerated sea-level change in recent years.8. Present state-of-the-art coupled climate models still cannot simulate many importantfeatures of major climate events like El Nino South oscillation and tropical and/or AsianMonsoon at this time. The climate models do not simulate many features of convective orlarge-scale precipitation characteristics.9. The Thermohaline Circulation in the North Atlantic has exhibited considerable variability inthe 20th century; however this variability appears to be part of natural multi-decadal climatevariability and does not appear to be linked to Global Warming.10. Future projections of earth’s climate using present climate models do not have sufficientreliability for climate policy decisions.http://friendsofscience.org/documents/Madhav%20bibliography%20SHORT%20VERSION%20Feb%206-07.pdfYou're nothing more than a sophist. [Edited on June 6, 2007 at 5:35 AM. Reason : .]
6/6/2007 5:25:45 AM
6/6/2007 11:27:57 AM
All the usefulness of this thread ended about 7-8 pages ago
6/6/2007 1:24:34 PM
^^ You're so goddamned stupid it's unbelievable. I shudder to think what kind of revisionist history indoctrination you may be subjecting young people to. Let's review how this exchange got started:
6/6/2007 2:55:45 PM
6/6/2007 3:16:15 PM
Oh, and since you seem to be in a mood to accept the word of scientists, here is the bibliography on just 1 of the sections of the IPCC study (the section on the climate models):This is just 1 of the 12 pages of references too, btw:
Abdalati, W., et al., 2001: Outlet glacier and margin elevation changes: Near-coastal thinning of the Greenland ice sheet. J. Geophys. Res., 106, 33729–33741. ACIA, 2004: Arctic Climate Impact Assessment (ACIA): Impacts of a Warming Arctic. Cambridge University Press, New York, NY, 140 pp. Adams, P.J., et al., 2001: General circulation model assessment of direct radiative forcing by the sulfate-nitrate-ammonium-water inorganic aerosol system. J. Geophys. Res., 106, 1097–1111. Allen, M.R., 1999: Do-it-yourself climate prediction. Nature, 401, 627. Allen, M.R., and W.J. Ingram, 2002: Constraints on future changes in climate and the hydrologic cycle. Nature, 419, 224–232. Allen, M.R., and D.A. Stainforth, 2002: Towards objective probabilistic climate forecasting. Nature, 419, 228. Allen, M.R., D.J. Frame, J.A. Kettleborough, and D.A. Stainforth, 2006a: Model error in weather and climate forecasting. In: Predictability of Weather and Climate [Palmer, T., and R. Hagedorn (eds.)]. Cambridge University Press, New York, NY, pp. 391–427. Allen, M.R., et al., 2000: Quantifying the uncertainty in forecasts of anthropogenic climate change. Nature, 407, 617–620. Allen, M.R., et al., 2006b: Observational constraints on climate sensitivity. In: Avoiding Dangerous Climate Change [Schellnhuber, H.J., et al. (eds.)]. Cambridge University Press, New York, NY, pp. 281–289. Alley, R.B., P.U. Clark, P. Huybrechts, and I. Joughin, 2005a: Ice-sheet and sea-level changes. Science, 310, 456–460. Alley, R.B., T.K. Dupont, B.R. Parizek, and S. Anandakrishnan, 2005b: Access of surface meltwater to beds of sub-freezing glaciers: Preliminary insights. Ann. Glaciol., 40, 8–14. Alley, R.B., et al., 2002: Abrupt Climate Change: Inevitable Surprises. US National Research Council Report, National Academy Press, Washington, DC, 230 pp. Amann, M., et al., 2004: The RAINS Model. Documentation of the Model Approach Prepared for the RAINS Peer Review 2004. International Institute for Applied Systems Analysis, Laxenburg, Austria, 156 pp. Ammann, C.M., G.A. Meehl, W.M. Washington, and C.S. Zender, 2003: A monthly and latitudinally varying volcanic forcing dataset in simulations of 20th century climate. Geophys. Res. Lett., 30, 1657. Andronova, N.G., and M.E. Schlesinger, 2001: Objective estimation of the probability density function for climate sensitivity. J. Geophys. Res., 106, 22605–22612. Annan, J.D., and J.C. Hargreaves, 2006: Using multiple observationally-based constraints to estimate climate sensitivity. Geophys. Res. Lett., 33, L06704, doi:10.1029/2005GL025259. Annan, J.D., J.C. Hargreaves, N.R. Edwards, and R. Marsh, 2005a: Parameter estimation in an intermediate complexity earth system model using an ensemble Kalman filter. Ocean Modelling, 8, 135–154. Annan, J.D., et al., 2005b: Efficiently constraining climate sensitivity with ensembles of paleoclimate simulations. Scientiic Online Letters on the Atmosphere, 1, 181–184. Arblaster, J.M., and G.A. Meehl, 2006: Contributions of external forcings to Southern Annular Mode trends. J. Clim., 19, 2896–2905. Arora, V.K., and G.J. Boer, 2001: Effects of simulated climate change on the hydrology of major river basins. J. Geophys. Res., 106, 3335–3348.Arzel, O., T. Fichefet, and H. Goosse, 2006: Sea ice evolution over the 20th and 21st centuries as simulated by current AOGCMs. Ocean Modelling, 12, 401–415. Ashrit, R.G., K. Rupa Kumar, and K. Krishna Kumar, 2001: ENSO-monsoon relationships in a greenhouse warming scenario. Geophys. Res. Lett., 28, 1727–1730. Ashrit, R.G., H. Douville, and K. Rupa Kumar, 2003: Response of the Indian monsoon and ENSO-monsoon teleconnection to enhanced greenhouse effect in the CNRM coupled model. J. Meteorol. Soc. Japan, 81, 779–803. Ashrit, R.G., A. Kitoh, and S. Yukimoto, 2005: Transient response of ENSO-monsoon teleconnection in MRI.CGCM2 climate change simulations. J. Meteorol. Soc. Japan, 83, 273–291. Austin, J., and N. Butchart, 2003: Coupled chemistry-climate model simulations for the period 1980 to 2020: Ozone depletion and the start of ozone recovery. Q. J. R. Meteorol. Soc., 129, 3225–3249. Bahr, D.B., M.F. Meier, and S.D. Peckham, 1997: The physical basis of glacier volume-area scaling. J. Geophys. Res., 102, 20355–20362. Banks, H., R.A. Wood, and J.M. Gregory, 2002: Changes to Indian Ocean subantarctic mode water in a coupled climate model as CO2 forcing increases. J. Phys. Oceanogr., 32, 2816–2827. Barnett, D.N., et al., 2006: Quantifying uncertainty in changes in extreme event frequency in response to doubled CO2 using a large ensemble of GCM simulations. Clim. Dyn., 26, 489–511. Bengtsson, L., K.I. Hodges, and E. Roeckner, 2006: Storm tracks and climate change. J. Clim., 19, 3518–3543. Beniston, M., 2004: The 2003 heat wave in Europe: A shape of things to come? An analysis based on Swiss climatological data and model simulations. Geophys. Res. Lett., 31, L02202. Berger, A., and M.F. Loutre, 2002: An exceptionally long interglacial ahead? Science, 297, 1287–1288. Berthelot, M., et al., 2002: Global response of the terrestrial biosphere to CO2 and climate change using a coupled climate-carbon cycle model. Global Biogeochem. Cycles, 16, 1084. Bertrand, C., J.P. Van Ypersele, and A. Berger, 2002: Are natural climate forcings able to counteract the projected global warming. Clim. Change, 55, 413–427. Bi, D.H., W.F. Budd, A.C. Hirst, and X.R. Wu, 2001: Collapse and reorganisation of the Southern Ocean overturning under global warming in a coupled model. Geophys. Res. Lett., 28, 3927–3930. Bindschadler, R., 1998: Future of the West Antarctic ice sheet. Science, 282, 428–429. Bitz, C.M., and G.H. Roe, 2004: A mechanism for the high rate of sea-ice thinning in the Arctic Ocean. J. Clim., 18, 3622–3631. Bitz, C.M., et al., 2006: The inluence of sea ice on ocean heat uptake in response to increasing CO2. J. Clim., 19, 2437–2450. Boer, G.J., and B. Yu, 2003a: Climate sensitivity and response. Clim. Dyn., 20, 415–429. Boer, G.J., and B. Yu, 2003b: Dynamical aspects of climate sensitivity. Geophys. Res. Lett., 30, 1135. Bond, T.C., et al., 2004: A technology-based global inventory of black and organic carbon emissions from combustion. J. Geophys. Res., 109, D14203, doi:10.1029/2003JD003697. B¨nisch, G., et al., 1997: Long-term trends of temperature, salinity, density, and transient tracers in the central Greenland Sea. J. Geophys. Res., 102, 18553–18571. Bony, S., and J.-L. Dufresne, 2005: Marine boundary layer clouds at the heart of cloud feedback uncertainties in climate models. Geophys. Res. Lett., 32, L20806, doi:10.1029/2005GL023851. Bony, S., et al., 2004: On dynamic and thermodynamic components of cloud changes. Clim. Dyn., 22, 71–86. Bony, S., et al., 2006: How well do we understand and evaluate climate change feedback processes? J. Clim., 19, 3445–3482. Bosilovich, M.G., S.D. Schubert, and G.K. Walker, 2005: Global changes of the water cycle intensity. J. Clim., 18, 1591–1608. Boucher, O., and M. Pham, 2002: History of sulfate aerosol radiative forcings. Geophys. Res. Lett., 29, L1308, doi:10.1029/2001GL014048. Box, J.E., et al., 2006: Greenland ice sheet surface mass balance variability (1988-2004) from calibrated Polar MM5 output. J. Clim., 19, 2783– 2800. Brabson, B.B., D.H. Lister, P.D. Jones, and J.P. Palutikof, 2005: Soil moisture and predicted spells of extreme temperatures in Britain. J. Geophys. Res., 110, D05104, doi:10.1029/2004JD005156. Bradley, R.S., F.T. Keimig, and H.F. Diaz, 2004: Projected temperature changes along the American cordillera and the planned GCOS network. Geophys. Res. Lett., 31, L16210, doi:10.1029/2004GL020229.
6/6/2007 3:16:43 PM
So, I'm stupid, I misspelled a word, and I used "2" twice in a list.Great rebuttal there.
6/6/2007 3:21:01 PM
6/6/2007 3:30:04 PM
3. Sea-level rise, ocean surface warming/cooling etc.Sea-level Risea. “New perspectives for the future of the Maldives” N-A Morner M Tooley & G Possnert Global andPlanetary Change 40 (2004) p. 177-182In the region of Maldives a general fall in sea-level rise occurred some 30 years ago.b. “Estimates of the regional distribution of sea-level rise over the 1950-2000 period” J A Church et alJ of Climate 17 (2004) p. 2609-2625Analyzes patterns of regional sea level rise over the period 1950-2000 and concludes thatit is not possible to detect a significant sea level rise over this period anywhere.c. “Low sea-level rise projections from mountain glaciers and icecaps under global warming” SarahRaper & Roger Braithwaite Nature V. 439 (2006) p. 311-313Projects sea level rise from mountain glacier and icecaps (outside of Greenland &Antarctic Ice Sheets) as only about 5.1 cm by 2100, half of previous projections.4d. “Nonlinear trends and multiyear cycles in sea-level records” S Jevrejeva et al J of GeophysicalResearch V.111(2006) C09012Obtains global sea level rise trend of 2.4 mm per year for the period 1993-2000e. “On the decadal rates of sea level changes during the twentieth century” S J Holgate GeophysicalResearch Letters 34 (2007) doi:10.1029/2006GL028492Analyses nine long and continuous records of sea level changes from 1904 through 2003.Sea level change of ~2.03 +/-.35 mm/yr from 1904-1953. 1954-2003, sea-level change isfound to be lower ~1.45 +/-.34 mm/yr.Ocean Surface Warming/Coolinga. “The sustained North American warming of 1997 and 1998” A Kumar et al J of Climate 14(2001)p.345-353Shows how the sustained North American land warming was primarily due to the intenseEl Nino event of 1997/98, which produced and maintained high sea surface temperaturevalues over the Pacific basin, as well as other ocean basins through the middle of 1998.b. “Recent cooling of the upper ocean” J Lyman J Willis & G Johnson Geophysical Research Letters33 (2006) L18604Documented cooling of the upper oceans and in particular of the southern north Atlantic.c. “Anomaly of heat content in the northern Atlantic in the last 7 years: Is the ocean warming orcooling?” V Ivchenko N Wells & D Aleynik Geophysical Research Letters 33 (2006) L22606Data from the Argo profiling buoys are analyzed for the North Atlantic, and found that thesouthern north Atlantic has cooled in the last seven years.d. “How much is the ocean really warming?” V Gouretski & K P Koltermann Geophysical ResearchLetters 34 (2007) L01610Studies global hydrographic data, as provided by bathythermographs, and found awarming bias when the bathythermographs data are compared against bottle and currenttemperature density data.4. Arctic & Antarctic temperatures: from Holocene to presenta. “First survey of Antarctic sub-ice shelf sediment reveals mid-Holocene ice shelf retreat” C J Pudsey& J Evans Geology 29 (2001) p.787-790Documents that the Larsen A & B ice shelves in the northeastern Antarctic Peninsula wereprobably altogether absent about two thousand years ago.b. “Antarctic climate cooling and terrestrial ecosystem response” P Doran et al Nature online 13January 2002 (DOI:10.1038/nature 710)Documents a cooling trend in the Antarctica using recent temperature data.c. “Variability and trends of air temperature and pressure in the maritime Arctic, 1875-2000” I VPolyakov et al J ournal of Climate 16 (2003) p. 2067-2077Presents a long series of temperature and pressure data (1875-2000) over the Arctic basin,and documents strong multi-decadal variability on a time scale of 50-80 years.d. “Holocene climate variability” P A Mayewski et al Quaternary Research 62 (2004) p. 243-255Identifies Rapid Climate Change throughout the Holocene, involving cool polar regionsand wet (or dry) tropical regions.e. Global warming & the Greenland ice sheets” P Chylek, J E Box & G Lesins Climatic Change (2004)63 p. 201-221Shows that a rapid warming over all of coastal Greenland occurred in the 1920s. Averageannual temperature rose between 2° and 4°C in less than ten years.f. “A multi-proxy lacustrine record of Holocene climate change on northeast Baffin Island, ArcticCanada” Quaternary Research (2006) 65 p. 431-442Shows a pronounced Holocene temperature maximum, about 5°C warmer than present.5g. “Greenland warming of 1920-1930 and 1990-2005” P. Chylek, M K Dubey & G Lesins GeophysicalResearch Letters 33 (2006) L11707Shows that a rapid warming over all of coastal Greenland occurred in the 1920s. Averageannual temperature rose between 2° and 4°C in less than ten years.h. “Extending Greenland temperature records into the late eighteenth century” B M Winter et al J ofGeophysical Research 111 (2006) D11105Extends Greenland temperature records back to the year 1784. The 1930s and the 1940swere the warmest decades, with 1941 as the warmest year.i. “Ice shelf history from petrographic and foraminiferal evidence, Northeast Antarctic Peninsula” C JPudsey et al Quaternary Science Reviews 25 (2006) p. 2357-2379Documents that the Larsen A & B ice shelves in the northeastern Antarctic Peninsula wereprobably altogether absent about two thousand years ago. Further concludes that the CO2concentration was about 100 ppm lower than at present.
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5. Impact of large-scale circulation patternsa. “A study of NAO variability and its possible non-linear influences on European surfacetemperatures” D Pozo-Vazquez et al Climate Dynamics, Vol. 17 (2001) p. 701-715Shows that a positive value of the north Atlantic oscillation index can produce winterseason warming in Europe.b. “Impacts of low frequency variability modes on Canadian winter temperature” B Bonsal, A Shabbar& K Higuchi Int’l journal of Climatology, Vol. 21 (2001) p. 95-108Shows how an El Nino event, together with positive values of the Pacific decadaloscillation index, can provide strong positive winter temperature anomalies over most ofCanada.c. “Are stronger North-Atlantic southwesterlies the forcing to the late-winter warming in Europe?” JOttermann et al Int’l J of Climatology, Vol. 22 (2002) p. 743-750Suggests that stronger south-westerlies in the North Atlantic may be producing earlyspring-like conditions in parts of Europe.d. “Variability of extreme temperature events in south-central Europe during the twentieth century andits relationship with large-scale circulation” P Domonkos et al Int’l J of Climatology, Vol. 23 (2003) p.987-1010Shows that a positive value of the north Atlantic oscillation index can produce winterseason warming in Europe.e. “January Northern Hemisphere circumpolar vortex variability and its relationship with hemispherictemperature and regional teleconnection” R Rohli, K Wrona & M McHugh Int’l J of Climatology, Vol.25 (2005) p. 1421-1436Discusses the circumpolar vortex and its linkage to both the Atlantic oscillation variability,and the Pacific North American pattern.6. Extraneous influence on mean temperature trends: urbanization, landusechange etc.a. “The influence of land-use change and landscape dynamics on the climate system: relevance toclimate-change policy beyond the radiative effect of greenhouse gases” R A Pielke sr et al Phil.Trans. R soc. London UK (2002)360 p.1705-1719Considered a landmark paper in the present global warming debate. This paper brings outan important aspect of land-use change and its dominating impact.b. “Impact of urbanization and land-use change on climate” E. Kalnay & M Cai, Nature, Vol. 423, 29May 2003, p. 528-531Using the National Centre for Atmospheric Research, USA, re-analyses upper-air data andan extrapolation to the surface, obtaining the urbanization impact on mean temperaturetrend to be about 0.280C over 100 years and about 0.180C over the recent 30 years.6c. “The urban heat island in winter at Barrow, Alaska” K Hinkel et al International J of Climatology, Vol.23, 2003, p. 1889-1905Obtains the urban-rural temperature difference of over 20C during the winter months atBarrow, Alaska.d. “Impacts of anthropogenic heat on regional climate patterns” A Block, K Keuler & E SchallerGeophysical Research Letters, Vol 31, L12211, 2004Shows how anthropogenic heat released from highly industrialized and populated areascan produce a permanent warming from 0.15° to 0.5°C.e. “A test of correction for extraneous signals in gridded surface temperature data” R McKitrick & PMichaels, Climate Research, Vol. 26, 2004, p. 159-173Documents a definite warm bias in the temperature trend, as a result of non-climaticimpact of local (and regional) economic activity.f. “Evidence for a significant urbanization effect on climate in China” L Zhou et al Proc. NationalAcademy of Science(USA) V. 101 (2004) p.9540-9544Obtains urbanization impact over China to be more than the estimated 0.27°C in the USAduring the 20th century.g. “Evidence for influence of anthropogenic surface processes on lower tropospheric and surfacetemperature trends” A T J De Laat & A N Maurellis, International J of Climatology, 26, 2006, p. 897-913Studies the influence of anthropogenic surface processes on mean temperature trends,estimated using green house gas emission world-wide database as proxy for industrialactivity. The mean temperature trends at highly industrial regions and locations werefound to be higher than elsewhere.h. “Urban heat island effect analysis for San Juan, Puerto Rico” A Velazquez-Lozada, J E Gonzalez &A Winter, Atmospheric Environment, 40, 2006, p. 1731-1741Documents a strong urban heat island effect at San Juan, Puerto Rico. It is estimated thatthe urban-rural temperature difference could increase to about 8°C by the year 2050.
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7. Uncertainties in climate model simulations of regional & global featuresa. “Potential role of solar variability as an agent for climate change” C Bertrand & J Van YperseleClimatic Change V 43 (1999) p.387-411It is shown that, although total solar irradiance reconstruction is insufficient to reproduceobserved warming of the 20th century, the model response suggests that the Gleissbergcycle (~88 yr) solar forcing should not be neglected in explaining the century-scale timevariations.b. “Simulated impacts of historical land-cover changes on global climate in northern winter” T N Chaseet al Climate Dynamics V 16 (2000) p. 93-10The simulations suggest that anthropogenic land cover changes can produce teleconnectionpatterns affecting global temperature and precipitation distributions.c. “Monsoon prediction-why yet another failure?” S Gadgil M Rajeevan & R Nanjundiah CurrentScience(India) V 88 (2005) P.1389-1400Examines prediction of the Indian monsoon for 2004 and conclude that the skill inforecasting the Indian summer monsoon variability has not improved in the last fifty yearsd. “Detection and attribution of twentieth-century northern & southern African rainfall change” MHoerling et al J of Climate V 19 (2006) p. 3989-4008Finds that the Sahel region drought of 1950-2000, was not influenced by the green housegas forcing, indicating that the Sahel drought conditions were likely of natural origin.e. “ENSO evolution and teleconnections in IPCC’s twentieth-century climate simulations: realisticrepresentation?” R Joseph & S Nigam J of Climate V 19 (2006) p.4360-4377Concludes that climate models are still unable to simulate many features of El Ninosouthern oscillation variability, its circulation and hydro-climatic tele-connections. Furtherthe climate system models are not quite ready for making projections of regional-tocontinentalscale hydro-climatic variability and change.7f. “Precipitation characteristics in eighteen coupled climate models” Aiguo Dai J of Climate V 19(2006) p.4605Concludes that considerable improvements in precipitation simulations are still desirablefor the latest generation of the world’s coupled climate models.g. “Is the thermohaline circulation changing?” M Latif et al J of Climate V 19 (2006) p.4631-4637Examines the thermohaline circulation in the North Atlantic, which is responsible for largeamounts of heat and freshwater transport by the Gulf Stream. Suggests the changes in thethermohaline circulation during the 20th century are likely to be the result of natural multidecadalclimate variability.8. Miscellaneous Studiesa. “Reconciling observations of global temperature change” Richard Lindzen & Constantine GiannitsisGeophysical Research Letters V 29 (2002) No 12 10.1029/2001GL014074Analyzes the discrepancy between global mean temperature trends, obtained by satellitemicrowave data, and surface temperature measurements.b. “Compilation and discussion of trends in severe storms in the United States: Popular perception vsclimate reality” Robert Balling Jr & Randall Cerveny Natural Hazards V 29 (2003) p. 103-112Documents the mismatch between popular perceptions, as created by media reports, andclimate reality, which does not show extreme weather as increasing in the USA.c. “On destructive Canadian Prairie windstorms and severe winters: A climatological assessment inthe context of global warming” Keith Hage Natural Hazards V 29 (2003) p. 207-228Documents a temporal frequency peak in severe windstorms and associated tornadoesduring the 1920s and 1930s, then a steady decline since 1940 through 1980s. A steep risein tornado frequency since 1970 is attributed to increasing awareness and reporting oftornado activity in recent years, and NOT due to change in tornado climatology.d. “Shifting economic impacts from weather extremes in the Unites States: a result of societalchanges, not global warming” Stanley Changnon Natural Hazards V 29 (2003) p. 273-290Documents that increasing economic impacts of extreme weather events in the USA is aresult of societal change and NOT global warming.e. “The global warming debate: A review of the present state of science” M L Khandekar T S Murty &P Chittibabu Pure & Applied Geophysics V 162 (2005) p. 1557-1586Concludes that the recent warming of the earth’s surface is primarily due to urbanization,land-use change, etc. and not due to increasing green house gas in the atmosphere.f. “Extreme weather trends vs dangerous climate change: A need for a critical reassessment” M LKhandekar Energy & Environment V 16 (2005) p.327-331Shows that extreme weather events like heat waves, winter blizzards, rainstorms, droughtsetc are not increasing anywhere in Canada, USA or elsewhere, where sufficient data areavailable for adequate analysis.g. “The interaction of climate change and the carbon dioxide cycle” A Rorsch R S Courtney & DThoenes Energy & Environment V 16 (2005) p. 217-238Argues the relatively large rise of CO2 in the 20th century, was caused by the increase inthe mean temperature which preceded it.h. “Can we detect trends in extreme tropical cyclones?” Christopher Landsea et al Science V 313(2006)p.452-454Suggests the Dvorak technique, developed to estimate hurricane strength, was notavailable in the late 1960s and early 1970s or before, when some of the hurricanes andtropical cyclones may have been stronger than estimated.i. “Trends in western North Pacific tropical cyclone intensity” M- C Wu K-H Yeung & W-L Chang EOSTransactions AGU V 87 (2006) No 48 28 November 2006Suggests that the western North Pacific tropical cyclone climatology does not revealincreasing strength for typhoon records from 1965 to 2004.8j. “On global forces of nature driving the earth’s climate: Are humans involved?” L F Khilyuk & G VChilinger Environmental Geology V 50 (2006) p. 899-910Presents a comprehensive review of the global forces driving the earth’s climate overgeological times. The present warming of the last 150 years is a short warming episode inthe earth’s geologic history. Human activity (anthropogenic green house gas emission)may be responsible for only 0.01°C of the approximately 0.56°C warming of the 20thcentury.http://friendsofscience.org/documents/Madhav%20bibliography%20SHORT%20VERSION%20Feb%206-07.pdf
6/6/2007 3:32:04 PM
Haha, that's funny.I take it that's your sign for defeat? Do you realize you are wrong now?
6/6/2007 3:35:27 PM
lol"You pointed out major flaws in my sources.To rebut, I'll quote them again, but in further detail.But I still won't actually read any of it."
6/6/2007 3:40:26 PM
^^ and ^ I'm not wrong--you two are just left-wing wack jobs that won't accept any relevant evidence, no matter how convincing. So go jerk each other in traffic, m'kay?[Edited on June 6, 2007 at 4:05 PM. Reason : .]
6/6/2007 4:05:26 PM
All you have to do is actually rebut our arguments,but, if you e-hate us that much, whatever. [Edited on June 6, 2007 at 4:07 PM. Reason : ]
6/6/2007 4:07:35 PM
6/6/2007 8:27:16 PM
Man, ya'll are really grasping at straws, here. Let's look at the quote again:
6/6/2007 9:02:16 PM
you don't get it. They could point to Ronald McDonald and claim that he represents the consensus, but that doesn't mean there is a consensus.try this one out. GhostHunters on Sci-Fi represents the scientific consensus that the earth is flat. Does that now mean there is a scientific consensus that the earth is flat?]
6/6/2007 9:40:42 PM
anything with IPCC in it I automatically disregard.
6/6/2007 9:41:54 PM
^^Do the Ghosthunters represent 16 national scientific academies?Are you not understanding that a joint statement of agreement by all major science academies represents a scientific consensus?Is there a single science academy that rejects anthropogenic climate change?^ As you should. If it's not some obscure scientist at an obscure Canadian university, you just can't trust it.
6/6/2007 9:45:13 PM
This thread has killed me. It has literally killed me. I am now dead because of the fact that this thread has gotten so motherfucking ridiculous.
6/6/2007 10:00:13 PM
^^I try to stay away from politically driven bullshit.^so true.
6/6/2007 10:44:12 PM
This thread is 23 pages?So, 5 pages of content, 3 pages of trolling, 2 pages of nothing, and 13 pages of repeating the first 5 pages, right?
6/6/2007 10:50:51 PM
SHUT THE FUCK UP, BLIND HATE, YOU STUPID CUNT
6/6/2007 10:52:53 PM
^^^ So the "Friends of Science" is not politically drive bullshit?And, what do you consider not-politically driven bullshit?Do you realize the IPCC report has 12 pages of bibliographies containing pre-existing (not commissioned by/for the IPCC) research on the issues relating to climate change?
6/7/2007 1:52:09 AM
6/7/2007 11:28:58 AM
Can people please stop with the name calling. It makes you look immature and weakens whatnever post you have. ^^I've looked over the IPCC report and don't feel like relooking that crap up over and over. Their main point with the "hockey stick" has already been severely disproven, what more do you need.
6/7/2007 1:23:57 PM
^ The name-calling? Probably not. At my age, I'm not concerned with looking mature. But I did think of a new slogan: The Wolf Web: Your Source for Maturity. Concerning my stand against groupthink, here's what the alarmists demand when you step out of line--even if you run NASA:NASA's Griffin regrets global warming remarks
6/7/2007 2:19:39 PM