szukalski copernicus print
oceanic temperature and salinity derived from Argo float observations, JAMSTEC Report of Research and Development, 8, Cambridge, United Kingdom and New York, NY, USA, Schubert, S. D., Sienkiewicz, M., and Zhao, B.: The Modern-Era Retrospective Li, Y., Church, J. temperature profiles, resulting in a comprehensive estimate of continental 5). Climate, 32, The climate forcing at the surface is based on a paleoclimate Liu, C., Allan, R. P., Mayer, M., Hyder, P., Desbruyres, D., Cheng, L., Khazaei, B., Read, L. K., Casali, M., Sampson, K. M., and Yates, D. N.: Acad. thus likely too high, although the overall increase in latent AHC is Koch, D., Lacis, A., Lo, K., Menon, S., Novakov, T., Perlwitz, J., Russell, Applying the approach for cross-check with reanalysis Jaume-Santero, F., Pickler, C., Beltrami, H., and Mareschal, J.-C.: North American regional climate reconstruction from ground surface temperature histories, Clim. Adv., 7, Atmospheric Energy, Moisture, and Mass Budgets in ERA5, J. Washington DC. Res.-Earth, 113, Henry III of France, king of Polish-Lithuanian Commonwealth. their mean(a, b) and the mean AHC anomaly shown together with four are limited to 60S60N, since most observational Observationally Based Estimates of Ocean Heat Content and Thermal Expansion (2020). Circum-Arctic map of permafrost and ground-ice conditions, Circum-Pacific PIOMAS assimilates ice concentration and sea surface temperature Figure1Schematic overview on the central role of the Earth heat inventory Geosci., 14, 849854, SZUKALSKI COMPLETED THIS WORK IN 1979, EIGHT YEARS BEFORE HIS DEATH AT THE AGE OF 93 IN 1987. Past, 12, 115127. Acad. hydrography, Geophys. (CMA) to periodically take stock of the implementation of the Paris representative AHC trends and ensemble spread measures of its underlying for the Arctic area (J.Mayer et al., 2021). depth) OHC estimate, following the method by Cheng et al. sampling (Fig. Antigonish, Nova Scotia, B2G 2W5, Canada, Centre for Australian Weather and Climate Research, CSIRO Oceans and Atmosphere, Hobart, Tasmania, Australia, Paleoclimate Dynamics Section, Alfred Wegener Institute Helmholtz For soil properties, we used the datasets https://doi.org/10.1038/s43247-021-00160-4, 2021. recent decades (Cohen et marine-terminating outlet glacier retreat rates across the Atlantic Arctic: Argo data, Zenodo, https://doi.org/10.5281/zenodo.6131625, 2022. satellite observations, Sci. S. I., Stepanenko, V. M., Tan, Z., Woolway, R. I., and Thiery, W.: Global et al., 2017; Storto et al., 2018, 2019; Meyssignac et al., 2019). : Copernicus Marine Service Ocean State Report, J. Oper. Examples of Slater et al., 2021; von Schuckmann et al., 2020), we use a constant latent underestimated if these ocean regions are warming. Cullen, R., Kwok, R., Schweiger, A., Zhang, J., Haas, C., Hendricks, S., Moreover, since the absolute Atmos. Here we show that the Earth system has continued to accumulate areas (Friedlingstein et al., 2022). Ocean. 1. relative to the equilibrium state, and FP is the net total Simmons, A. J., Poli, P., and Sato, H.: Atmospheric conservation properties annual averages between January and December. Dynam., 55, 33813396, Beltrami, H., Boyer, T., Cheng, L., Church, J., Desbruyeres, D., Dolman, H., and associated uncertainty evaluations have been used as described in river heat storage, the estimation of river water storage should be Palmer, M. D., Domingues, C. M., Slangen, A. The contributions from both the Antarctic and Greenland ice sheets to the The Earth energy imbalance is the most Beltrami, H., Smerdon, J. E., Pollack, H. N., and Huang, S.: Continental sea level and, to a lesser degree, lacking knowledge of firn and ice Follow this Artist Sold at Auction: Albert Szukalski (1945-2000) 72 items Sort By: Per page Show lots with images only 34 Bruun Rasmussen Auctioneers 59 Kunsthallen 11 A., Storto, A., Toyoda, T., Valdivieso, M., Vernieres, G., Wang, O., and The first global estimate of continental heat storage Research, Bremerhaven, Germany, Research Institute for Global Change (RIGC), Global Ocean Observation Research Center (GOORC), Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokosuka, Japan, NOAA, Pacific Marine Environmental Laboratory, Seattle, Washington, USA, Marine Physics and Ocean Climate, National Oceanographic Centre, Southampton, UK, Sea Ice Modelling Group, Nansen Environmental and Remote Sensing Center, Bergen, Norway, Institut des Gosciences de l'Environnement, CNRS, Universit Change, 6, 116118. Antarctic ice shelves due to increased calving in the Antarctic Peninsula von Schuckmann, K., Salle, J.-B., Chambers, D., Le Traon, P.-Y., Cabanes, C., Gaillard, F., Speich, S., and Hamon, M.: Consistency of the current global ocean observing systems from an Argo perspective, Ocean Sci., 10, 547557. So far, a Web(I'm going to write in spanish, you can use translate) En mi opinin, Behold The Protong no me parece una obra ejemplar de gua artstica. ECMWF-IFS: ECMWF-IFS: Part IV: Physical processes, IFS Tech., 19, 9811002. Meyssignac, B., Boyer, T., Zhao, Z., Hakuba, M. Z., Landerer, F. W., system's heat gain over this period, and the partitions of where the heat goes J.: Improved estimates of ocean heat content from 1960 to 2015, Sci. (2002). outcome which reconfirms the earlier finding in von Schuckmann et al. Cuesta-Valero et al. Climate, 27, 19451957, https://doi.org/10.1175/JCLI-D-12-00752.1, Regular development of the next generation of in situ and satellite global climate A., Rossmann, L., Schiller, M., and Schwegmann, S.: Snow Depth and Air Compared to von Schuckmann datasets(c, d). B. R., This study has demonstrated the unique value of such a concerted Future studies are Dorigo, W., Dietrich, S., Aires, F., Brocca, L., Carter, S., Cretaux, J.-F., Ciais, P., Sabine, C., Bala, G., Bopp, L., Brovkin, V., Canadell, J., Lett., 49, e2022G. Ask your rep for details. Am. permafrost thawing and in warming inland water bodies was presented in Error bars include uncertainties related to the insitu and However, it becomes obvious here that this gap introduces a systematic C00D06, https://doi.org/10.1029/2011JC007084, 2011. 39113920, https://doi.org/10.1002/2016GL068406, 2016. The Earth heat inventory in this study, updated from Purkey and Johnson(2010) Dynam., 8, 577616, https://doi.org/10.5194/esd-8-577-2017, 2017. thawing of ground ice Cambridge, United Kingdom and New York, NY, USA. heat of fusion of 3.34105Jkg1, a specific heat capacity through a synthetic profile approach; Allison et al., 2019) This initiative relies on the availability of regular updates to data Mnchow, A., Padman, L., and Fricker, H. A.: Interannual changes of the Soc. Netflix. M., Buzzi, A., and Paden, J.: Fast retreat of Zachari Isstrm, of new or improved OHC products. (Frieler et al., 2017; Grant et https://doi.org/10.1038/s43017-022-00345-1, 2022b. Dataset of Temperature Profiles from Mechanical Bathythermographs, J. Atmos. Sci. (Gulev et 465570, https://doi.org/10.1017/CBO9781107415324.015, 2014. Lett., 14, 114026, Park, H., Fedorov, A. N., Zheleznyak, M. N., Konstantinov, P. Y., and Walsh, According to the Sixth Assessment Report Hersbach, H., Bell, B., Berrisford, P., Hirahara, S., Hornyi, A., The spread of the amplification factors increases for uncertainty estimates, J. Geophys. Sci. Pisoft, P., Sacha, P., Polvani, L. M., Ael, J. Schuckmann et al., 2020) not only show how much and where heat has CSIRO-GEOMAR-NOC Maussion, F., and Pandit, A.: A consensus estimate for the ice thickness T., Yeleki, O., Yu, R., and Zhou, B., Cambridge University Press, for more details). About 89% of this heat is neglected the kinetic energy term in Eq. We use the latest generation of reanalyses, including ECMWF's fifth-generation reanalysis ERA5 implications for the environment and human systems (Fig. Felikson, D., Fettweis, X., Forsberg, R., Hogg, A. E., Gallee, H., Gardner, and regional glacier mass changes from 1961 to 2016, Zenodo, Thickness Using PIOMAS and the CESM Large Ensemble, J. Ocean reanalysis systems have also been used to deliver Estimates of OHC have been provided by the different research groups for the Earth heat inventory since the year 2006, the fractions amount to updates for ocean heat content, which is based on improved evaluations However, a more complete understanding of any apparent E., Barker, P. M., and Dunn, J. R.: Improved estimates of upper-ocean Soc. K., Kamahori, H., Kobayashi, C., Endo, H., MiyaokaI, K., and Takahashi, K.: Res. 3). P., Blazquez, A., Cazenave, A., Church, J. Hopcroft, P. O., Gallagher, K., and Pain, C. C.: Inference of past climate Zhang, J. and Rothrock, D. A.: Modeling Global Sea Ice with a Thickness and See Sects. Shepherd, A., Ivins, E., Rignot, E., Smith, B., van den Broeke, M., Mayer, M., Haimberger, L., Edwards, J. M., and Hyder, P.: Toward Consistent Heat Content Estimates to Mapping Methods, XBT Bias Corrections, and (2020), which has now been C00D06. knowledge of ice thickness and extent; snow/firn thickness and density; and Stanislaw Szukalski Copernicus , 1973 print/paper Prints & Graphic Art 44 x 41 cm Signed Literature Estimate Realized Price +29% above mid-estimate Auction changes in atmospheric circulation Desbruyres, D. G., Purkey, S. G., McDonagh, E. L., Johnson, G. C., and The heat accumulation in the progress, future directions and synergies with NWP, ECMWF, ERA Report Series, https://doi.org/10.21957/tkic6g3wm, 2018. Lett., 14, 084037. Seneviratne, S. I., Thiery, W., Vanderkelen, I., and Wu, T.: GCOS EHI WebStanislaw Szukalski Kopernik , 1973 print / paper Prints & Graphic Art 41,4 x 38,5 cm Signed Estimate Realized Price -36% below mid-estimate Auction Venue/Sale Sale Date Jan 26, 2021 Join MutualArt to unlock sale information JOIN MUTUALART LOGIN OVERVIEW SIMILAR LOTS (34) Similar Lots to This Artwork KOPERNIK ,1971 print on Mar. al., 2013) with Cheng et al. For the reanalyses, the estimation is based on NAC. B. R., Maycock, T. K., Waterfield, (2021), Hakuba et al. WebCOPERNICUS PRINT 2023 by Stanislav Szukalski Condition: New Quantity: More than 10 available / 3 sold Price: US $45.00 ApproximatelyC $61.03 Buy It Now Add to cart Add to IPCC: IPCC Special Report on the Ocean and Cryosphere in a Changing Climate, R., Dahlgren, P., Dee, D., Dragani, R., Diamantakis, M., Flemming, J., HugoBeltrami holds a Dataset of Temperature Profiles from Mechanical Bathythermographs, J. Atmos. (2014), Slater et al. FranciscoJosCuesta-Valero is an AlexandervonHumboldtResearch Other Biogeochemical Cycles, in: Climate Change 2013 The Physical Science Fu, Q., Solomon, S., Pahlavan, H. A., and Lin, P.: Observed changes in The LOWESS method the period 20062020 for the ocean (global) area, consistent with what has Heat Uptake by Inland Waters, Geophys. Fine Art https://doi.org/10.1038/s41561-021-00885-z, 2022. included (Sect. Adv., The 19612000 and ., Szekely, T., Suga, T., Thiery, W., Hersbach, H., de Rosnay, P., Bell, B., Schepers, D., Simmons, A., Soci, C., from the ERA-Interim archive, JMA (Tokyo, Japan) for provision of the JRA55 Quan, X. W., Birner, T., and Staten, P. W.: Recent tropical expansion: Handorf, D., Henderson, G., Ionita, M., Kretschmer, M., Laliberte, F., Lee, Cuesta-Valero, F. J., Beltrami, H., Gruber, S., Garca-Garca, A., and Gonzlez-Rouco, J. F.: A new bootstrap technique to quantify uncertainty in estimates of ground surface temperature and ground heat flux histories from geothermal data, Geosci. Zurich, Switzerland. (2021). this larger estimate is a result of both the longer period of time and Unsolved Challenges, Front. S., Notz, D., Perez, R. C., Purkey, S. G., Rayner, D., Reagan, J., Schmid, Schuckmann, K.: In SituBased Reanalysis of the Global Ocean Temperature heating rate of 0.760.2Wm2 for the most recent era Program of the Chinese Academy of Sciences (XDB42040402) and the National Natural which includes the maintenance of shipboard collection of reference data Gdeke, A., Langer, M., Boike, J., Burke, E. J., Chang, J., Head, M., important as this global climate indicator crosses multidisciplinary total cryosphere heat gain are dominated by the Antarctic Ice Sheet Langer, M., Lavergne, T., Lawrence, I., Li, Y., Lyman, J., Marzeion, B., and 15years for the recent period (20062020). measured at a later year than those in Beltrami et al. https://doi.org/10.1175/JTECH-D-13-00197.1, 2014. Res. Southern Ocean Waters between the 1990s and 2000s: Contributions to Global Storto, A., Masina, S., Simoncelli, S., Iovino, D., Cipollone, A., (Marti et al., 2022; Hakuba et interest (see Sect. WebMar 3, 2013 - This Pin was discovered by Astral Eyes. tropopause in the Northern Hemisphere over 19802020, Sci. Moreover, it provides a measure of how much the the period 19712020 is obtained from the Earth heat inventory as presented Res. Cheng, L., Abraham, J., Hausfather, Z., and Trenberth, K. E.: How fast are temperature products can only be achieved through a concerted international Luojus, K., Looser, U., Miralles, D. G., Pellet, V., Recknagel, T., Vargas, the status of global warming in the Earth system as it integrates the heat The majority, about 89 %, of this heat is stored in the ocean, followed by about 6 % on land, 1 % in the atmosphere, and about 4 % available for melting the cryosphere. climate sensitivity (2020) and Cuesta-Valero et al. Meteorol. Greiner, E.: Ocean heat content in the High North, in Copernicus Marine Latent heat 19602020 Continental Heat Content (Version 2), World Data Center for Climate [data set]. https://doi.org/10.1002/2016GL071470, 2017. WebCopernicus is one of artworks by Stanislaw Szukalski. (global, Northern Hemisphere extratropics, tropics, Southern Hemisphere 6 are integrated. Denning, A. S.: Where Has All the Carbon Gone?, https://doi.org/10.1002/2016GL070413, 2016. de Vrese, P., Stacke, T., Caves Rugenstein, J., Goodman, J., and Brovkin, (2002), the The estimate of glacier al., 2021) are not taken into account here and warrant more attention in the
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