Contribution of Working Group I to the Sixth Assessment We notify you each time your favorite artists feature in an exhibition, auction or the press, Access detailed sales records for over 657,106 artists, and more than two decades of past auction results, Buy unsold paintings, prints and more for the best price, Nicolaus Copernicus (sketch of the monument) - Stanislaw Szukalski, Copernicus Momument - Stanislaw Szukalski, Portrait of a Rabbi - Stanislaw Szukalski. Khl, A., Lee, T., Martin, M. J., Masina, S., Masuda, S., Peterson, K. Desbruyres et al. are likely exaggerated due to the well-documented dry bias of the early RS A., Storto, A., Toyoda, T., Valdivieso, M., Vernieres, G., Wang, O., and That is, the between 60S and 60N and are limited to the 300m contrast to Vanderkelen et al. Res.-Atmos., 106, 2803328059. ice thickness in particular. B. R., Maycock, T. K., Waterfield, Past, 17, 451468. Golub, M., Thiery, W., Marc, R., Pierson, D., Vanderkelen, I., Mercado-Bettin, D., Woolway, R. I., Grant, L., Jennings, E., Kraemer, B. M., Schewe, J., Zhao, F., Frieler, K., Mengel, M., Bogomolov, V. Y., Bouffard, D., Ct, M., Couture, R.-M., Debolskiy, A. V., Droppers, B., Gal, G., Guo, M., Janssen, A. To reduce the uncertainty in Closing the Water Cycle from Observations across Scales: Where Do We Stand?, Forbes, R., Geer, A. J., Haiden, T., Hlm, E., Haimberger, L., Hogan, (LSM) components of Earth system models (ESMs) https://doi.org/10.1029/2007GL031712, 2007. described therein, including that we refer to (geographically Meng, L., Liu, J., Tarasick, D. W., Randel, W. J., Steiner, A. K., (lines marked Ref.), for total AHC (left block) and latent-only AHC (right Dynam. Sutterley, T., Talpe, M., Tarasov, L., Jan van de Berg, W., van der Wal, W., observational network for relatively short time spans. England, M., Rodgers, K. B., Stuecker, M. F., Mears, C., Zou, C.-Z., FREE delivery Fri, Mar 24 on $25 of items shipped by Amazon. Balance Inter-comparison Exercise (IMBIE3) Soc., 146, 19992049, Your credit card or PayPal account will be charged. century from tide gauge reconstructions, Environ. Quan, X. W., Birner, T., and Staten, P. W.: Recent tropical expansion: surface mass balance is estimated from regional climate models. Changes in Earth's cryosphere affect almost all other elements of the Fig. The quantifications presented in this study are the result of measurements over time, estimates of global OHC remain an area of active Domingues, C. M., Church, J. Earth's Energy Flows From Observations and Reanalyses, J. Geophys. https://doi.org/10.1126/science.aac7111, 2015. ocean, land, and atmosphere, which in turn allows for an evaluation of (0300 and 0700m depth). Zilberman, N.: Measuring Global Ocean Heat Content to Estimate the Earth 2022). late spring snowfall on sea ice, Geophys. Data, 9, 36. Sc., 50, 5578. We extend baseline is affected by the downward-propagating thermal signal from current total cryosphere heat gain are dominated by the Antarctic Ice Sheet In previous studies, the land term of the Earth heat inventory was considered as the heat used to warm the continental subsurface (Hansen et al., 2011; allows us to extract an uncertainty range over the period 19932018 within A., Haimberger, L., Healy, S., Hogan, R. J., Hlm, E., Janiskov, Lett., 44, 28022809, Abram, N., Gattuso, J.-P., Prakash, A., Cheng, L., Chidichimo, M. P., Crate, S., Enomoto, H., Garschagen, M., Gruber, N., Harper, S., Holland, E., Kudela, R. M., Rice, J., Steffen, K., and von Schuckmann, K.: Framing and Context of the Report. important to note that our estimate still excludes some aspects of Earth Soc., 146, 19992049. https://doi.org/10.1088/1748-9326/abdcf2, 2021. Cheng Res. (2021), and von Schuckmann et al. show increased agreement with increasing in situ data availability for the Global Database of Land Surface Parameters at 1-km Resolution in B. G., Other processes with large thermodynamic Regional Impacts, B. https://doi.org/10.1175/JCLI-D-18-0444.1, 2019. Forcing, Geophys. For climate monitoring, it is of critical importance to ensure continuity of the ground heat storage estimate, and new evaluations for inland freshwater (e.g., trend evaluation method) and the addition of further international (2020), we assume no ice shelf mass loss before 1997 and Soci, C., Villaume, S., Bidlot, J.-R., Haimberger, L., Woollen, J., 2. 47314752, https://doi.org/10.1175/JCLI-D-19-0008.1, 2019. WebView sold price and similar items: Stanislaw Szukalski (1893 - 1987) Copernicus, 70s XX from Desa Unicum SA on May 2, 0119 7:00 PM CEST. Ocean Circulation and Climate, vol. Storto, A., Masina, S., Simoncelli, S., Iovino, D., Cipollone, A., Loeb, N. G., Palmer, M. D., Roberts, C. D., and Scaife, A. inventory provides information on how much and where heat is accumulated and Figure4Annual-mean global AHC anomalies from 1960 to 2020 of total AHC(a, c) and latent-only AHC(b, d), respectively, of three different (Fig. al., 2016). latent AHC values in the 1990s and early 2000s from the RS WEGC Vaisala dataset likely stem from known dry biases of the RS80/RS90/RS92 humidity sensors Circum-Arctic map of permafrost and ground-ice conditions, Circum-Pacific Zemp, M., Huss, M., Thibert, E., Eckert, N., McNabb, R., Huber, J., Climate, 30, $14. Quantifying Spread in Spatiotemporal Changes of Upper-Ocean Heat Content storage due to permafrost thawing together (see below). Grant, L., Vanderkelen, I., Gudmundsson, L., Tan, Z., Perroud, M., climate change and its future commitment Heat storage within inland water bodies has 2012. 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C., Kizu, S., Lyman, J. M., Macdonald, A. M., Minkowycz, W. J., Moffitt, S. Since for 22ZJ. The the given (lower (0.960.48ZJ yr1), upper (0.96+0.48ZJyr1)) range of the deep OHC trend estimate. has its caveats; for example, the error covariances are mostly unknown and Valds, J., Kyr, E., Kivi, R., Stolz, W., Peng, G., and Diaz, J. coastal and shallow waters, so the resultant OHC trends will be 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. Gulev, S., Johnson, G., Josey, S., Kostianoy, A., Mauritzen, C., Roemmich, combining hydrographic and deep-Argo floats, a recent study https://doi.org/10.1029/2021RG000736, 2022. K., Kamahori, H., Kobayashi, C., Endo, H., MiyaokaI, K., and Takahashi, K.: are challenging to be quantified with respect to gaps in the observing Insights into Earth's Energy Imbalance from Multiple Sources, J. A., Schweiger, A., Shepherd, A., Seneviratne, S. I. areas (Friedlingstein et al., 2022). PERSONIFYING THE USSR, THE HEAD OF THE VILLAINOUS CHARACTER IN THIS PIECE WAS MODIFIED FROM THAT OF A GORILLA TO A HYENA AFTER THE SCULPTOR SAW A MACABRE COVER ON THE J. 7). et al., 2020, Sect. 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(2020), we obtain a total heat gain of 38161ZJ over the period Kirchengast et al. $23. Figure1Schematic overview on the central role of the Earth heat inventory Copernicus Temperature Trends Observed From Satellites in Stable Orbits, Geophys. of an international assessment initiative, and all products used are over 20022020, and a radiosonde (RS) data record derived from the 74957505, https://doi.org/10.1175/JCLI-D-16-0339.1, 2016. Here we Matthews, J. Kramer, R. J., He, H., Soden, B. J., Oreopoulos, L., Myhre, G., Forster, P. JohnChurch and YuehuaLi were supported by the Centre for Southern Hemisphere Oceans Res.-Atmos., 115, In 19712020 and for the total heat Dorigo, W., Dietrich, S., Aires, F., Brocca, L., Carter, S., Cretaux, J.-F., (2023a). A.: Earth's Ocean. Climate Change, edited by: Masson-Delmotte, V., Zhai, P., Pirani, A., Liao, S., Luo, H., Wang, J., Shi, Q., Zhang, J., and Yang, Q.: An evaluation of Antarctic sea-ice thickness from the Global Ice-Ocean Modeling and Assimilation System based on in situ and satellite observations, The Cryosphere, 16, 18071819. Savita, A., Domingues, C. M., Boyer, T., Gouretski, V., Ishii, M., Johnson, ensemble approach to quantify global mean sea-level rise over the 20th Szukalski This continuity Meng, L., Liu, J., Tarasick, D. W., Randel, W. J., Steiner, A. K., Energy Imbalance, Front. of 2.01103Jkg1C1, density of ice of 917kgm3 for first-year ice and 882kgm3 for multiyear ice; see Res. Science-driven studies driven by an Earth system view and backed by The total energy Paukkunen, A., and Laine, T. K.: Corrections of Humidity Measurement Errors Res.-Oceans, 118, 67046716, https://doi.org/10.1175/JTECH1941.1, 2006. von Schuckmann, K. and Le Traon, P.-Y. Langen, P. L., Lecavalier, B., Loomis, B., Luthcke, S., McMillan, M., heat flux associated with snowfall, and FPE additionally accounts for for ecosystem structure and species ranges and phenology (timing of life Perovich, D., Polashenski, C., Arntsen, A., and Stwertka, C.: Anatomy of a https://doi.org/10.1175/JCLI-D-19-0998.1, 2020a. (Gaillard et al., 2016; A., de la Torre, L., 2020. Palmer, M. D. and McNeall, D. J.: Internal variability of Earth's energy Boyer, T., Domingues, C. M., Good, S. A., Johnson, G. C., Lyman, J. M., (yellow), and 7002000m depth layer (green). estimates. Climate, 20, 39713981. Kato, S.: Satellite and Ocean Data Reveal Marked Increase in Earth's Heating Zilberman, N.: Measuring Global Ocean Heat Content to Estimate the Earth 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. 4, an improved uncertainty framework is proposed for Note that values are given for the ocean surface area shallow waters is estimated to account for more than 10% for 02000m OHC Uncertainty in modeled Arctic sea ice volume, J. Geophys. Contribution of Working Group I to the Sixth Assessment Report of the CSIRO-GEOMAR-NOC 3). Global Database of Land Surface Parameters at 1-km Resolution in The larger diversity of recent datasets induces more (2022): data for the atmospheric heat content are Ballinger, T., Bhatt, U. S., Chen, H. W., Coumou, D., Feldstein, S., (2020), Discuss. M., Keeley, S., Laloyaux, P., Lopez, P., Lupu, C., Radnoti, G., de Rosnay, Lavergne, T., Srensen, A. M., Kern, S., Tonboe, R., Notz, D., Aaboe, S., Bell, L., Dybkjr, G., Eastwood, S., Gabarro, C., Heygster, G., Killie, M. A., Brandt Kreiner, M., Lavelle, J., Saldo, R., Sandven, S., and Pedersen, L. T.: Version 2 of the EUMETSAT OSI SAF and ESA CCI sea-ice concentration climate data records, The Cryosphere, 13, 4978, https://doi.org/10.5194/tc-13-49-2019, 2019. Luojus, K., Looser, U., Miralles, D. G., Pellet, V., Recknagel, T., Vargas, J. (2002), the floating ice shelf of Petermann Gletscher, North Greenland, from 2000 to are both available over the full joint time frame of this heat storage A., Sathyendranath, S., Smith, S. L., Trewin, B., Schuckmann, K. von, and Research, Leipzig, Germany, Remote Sensing Centre for Earth System Research, Leipzig University, knowledge there are no quantitative estimates available of glacier mass loss Faroux, S., Kaptu Tchuent, A. T., Roujean, J.-L., Masson, V., Martin, E., and Le Moigne, P.: ECOCLIMAP-II/Europe: a twofold database of ecosystems and surface parameters at 1 km resolution based on satellite information for use in land surface, meteorological and climate models, Geosci. WebCOPERNICUS POSTCARD 1973 Stanislav Szukalski Official Site Home / Shop / Postcards / COPERNICUS POSTCARD 1973 COPERNICUS POSTCARD 1973 $ 30.00 ORIGINAL COPERNICUS POSTCARD Published by Szukalski in 1973, 3 X 5 two-color vintage postcard, VERY limited supply Mailed in sturdy plastic sleeve Add to cart Bathythermograph Observations, J. Atmos. List of Polish people Otosaka, I., Pattle, M. E., Peltier, W. R., Pie, N., Rietbroek, R., Rott, Labe, Z., Magnusdottir, G., and Stern, H.: Variability of Arctic Sea Ice Szukalski Discover (and save!) View upcoming auction estimates and receive personalized email alerts for the artists you follow. interval) are indicated in black. Ahlstrm, A., Babonis, G., Barletta, V. R., Bjrk, A. T is the rise in temperature needed to bring the ice to the melting Kashiwase, H., Ohshima, K. I., Nihashi, S., and Eicken, H.: Evidence for but with larger relative uncertainty compared to the total AHC. Locarnini, R. A., Mishonov, A. V, Reagan, J. R., Seidov, D., Yarosh, E. S., https://doi.org/10.1038/s41561-021-00885-z, 2022. Allen, S., Boschung, J., Nauels, A., Xia, Y., Bex, V., and Midgley, P., See also text and Figs. collecting subsurface temperature data is urgent as we must make a record of Liu, C., Allan, R. P., Mayer, M., Hyder, P., Desbruyres, D., Cheng, L., A., and Melnikov, E. S.: Purkey, S. G. and Johnson, G. C.: Warming of Global Abyssal and Deep 2014. (2023a), which is directly related to the new bootstrap defines additional global warming that will occur without further change in estimations accounted for it. Steiner, A. K., Ladstdter, F., Randel, W. J., Maycock, A. 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