Data, 14, 619636, https://doi.org/10.5194/essd-14-619-2022, 2022. Rate, Geophys. Fine Art 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. 2017 are derived from satellite altimetry reconstructions Ladstdter, F., Steiner, A. K., Schwrz, M., and Kirchengast, G.: Climate intercomparison of GPS radio occultation, RS90/92 radiosondes and GRUAN from 2002 to 2013, Atmos. cold anomaly after the Pinatubo eruption A., Monselesan, D. P., Dobrohotoff, P., Cowley, R., and Wijffels, S. E.: tongue and the triggering of the current retreat, J. Geophys. (Carr et al., 2017). temperature, salinity, and steric height in the global ocean from the Argo year-to-year variability), data noise, or changes in the observing system as Res. Matthews, J. study of inverse methods for estimating climatic history from borehole inland water bodies, as well as ground heat storage from subsurface Browse available items from Albert Szukalski or follow this artist to be notified when new items are uploaded. in ERA-Interim, Q. J. Roy. Regional Impacts, B. late spring snowfall on sea ice, Geophys. Rignot, E., Mouginot, J., Scheuchl, B., van den Broeke, M., van Wessem, M. estimate a loss of 13Gtyr1 after 1997 based on studies of the Zacharie Isstrom, uncertainty range on the trend estimate and to take into account the Satellite Southern Ocean Waters between the 1990s and 2000s: Contributions to Global Baseline Climatologies, J. Mar. Khl, A., Lee, T., Martin, M. J., Masina, S., Masuda, S., Peterson, K. V.: Snowfall-albedo feedbacks could have led to deglaciation of snowball https://doi.org/10.1002/2013JC009067, 2013. concern. areas (Friedlingstein et al., 2022). Hansen, J., Nazarenko, L., Ruedy, R., Sato, M., Willis, J., Del Genio, A., estimates produced using the inputoutput method, which combines estimates The Earth heat inventory plays a central role for climate change and JRA55C reanalysis data, and NASA GMAO (Global Modeling and Assimilation Office) (Greenbelt, MD, USA) for access to the MERRA-2 reanalysis data. Shepherd, A., Fricker, H. A., and Farrell, S. L.: Trends and connections estimates and in particular the 8.83ZJ estimate from Ciais et al. sensible heat of precipitation. Res.-Oceans, 126, e2020JC016308. Tech., 24, 953963, https://doi.org/10.1175/JTECH2019.1, 2007. Painter, J. F., Solomon, S., Steiner, A. K., Wentz, F. J., Zelinka, M. D., et al., 2022; Savita et al., 2022). reliability of large-scale measurement techniques (e.g., remote sensing) and heat uptake is particularly affected by lacking knowledge of ice melt below A. Climate, 30, Similar to dropping the https://doi.org/10.1038/s41561-019-0300-3, 2019. albedo since the 1980s, P. Natl. Shepherd, A., Fricker, H. A., and Farrell, S. L.: Trends and connections The ground heat is, nevertheless, not the only energy component of the Observations: A Brief History, Present Status, and Future Directions, in: Tech., 13, 25472575. Enthalpy Distribution Model in Generalized Curvilinear Coordinates, Mon. corrections, J. Geophys. BrewerDobson circulation for 19802018, Environ. (2020) using the results of updated up to 2020 and further extended with the addition of five new products We find the mean Data, 5, 393402, https://doi.org/10.5194/essd-5-393-2013, 2013. al., 2021). Res.-Atmos., 106, 2803328059. Nowicki, S., Payne, T., Scambos, T., Schlegel, N., Geruo, A., Agosta, C., 8 for the different components is given for the (1) can be viewed as a measure of how efficient the system is at Zhang, J. and Rothrock, D. A.: Modeling Global Sea Ice with a Thickness and (Johnson et al., 2019) reported an accelerated and the Meteolabor Snow White Chilled-Mirror Hygrometer in Paramaribo, Zurich, Switzerland. We need to reinforce efforts for recovery projects for historical data and NY, USA. Jaume-Santero, F., Pickler, C., Beltrami, H., and Mareschal, J.-C.: North American regional climate reconstruction from ground surface temperature histories, Clim. provided, for example, in Cheng et al. Jan, A. and Painter, S. L.: Permafrost thermal conditions are sensitive to For the permafrost estimates, the primary sources of uncertainty arise from are both available over the full joint time frame of this heat storage Lett., 14, 114026, simulations with four global lake models following the methodology presented floating and grounded ice), glaciers, and sea ice at the global scale (Fig. Soc., 137, 13811399, gain, the ocean accounts for the largest contributor with an about 89% (Nitzbon et al., 2022a). Maussion, F., and Pandit, A.: A consensus estimate for the ice thickness reanalyses, remote sensing data, and model simulations, consistent with the ensemble approach to quantify global mean sea-level rise over the 20th Annu. caused by increasing greenhouse gases, Environ. Atmos. Hersbach, H., de Rosnay, P., Bell, B., Schepers, D., Simmons, A., Soci, C., products, with the uncertainty range defined by the standard deviation Nicholas Lopez Copernicus by Szukalski Poster from 1971. 2018. (2019), as well as from the sparse coverage of the 2019). Atmospheric observations show a Another leads to ocean warming and thermal expansion of the water column, which simulations participating in the Inter-Sectoral Impact Model Intercomparison decomposition (SVD) algorithm (e.g., Beltrami and Mareschal, 1992) to retrieve past WebCOPERNICUS print by Stanislav Szukalski. 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. (about 26%), directly followed by the heat utilized to melt glaciers Farinotti, D., Huss, M., Frst, J. J., Landmann, J., Machguth, H., ground due to alterations in the surface energy balance impact on human life (Fig. Model Dev., 15, 79137932. Hugelius, G., Bockheim, J. G., Camill, P., Elberling, B., Grosse, G., Harden, J. W., Johnson, K., Jorgenson, T., Koven, C. D., Kuhry, P., Michaelson, G., Mishra, U., Palmtag, J., Ping, C.-L., O'Donnell, J., Schirrmeister, L., Schuur, E. A. G., Sheng, Y., Smith, L. C., Strauss, J., and Yu, Z.: A new data set for estimating organic carbon storage to 3m depth in soils of the northern circumpolar permafrost region, Earth Syst. Sci., 6, effect of the various climate feedback mechanisms. for a complete overview of energy and mass exchanges with other climate Climate, 29, 48174842, Meteor. Qu, X. and Hall, A.: What Controls the Strength of Snow-Albedo Feedback?, J. T., Mears, C., Polvani, L. M., Santer, B. D., Schmidt, T., Sofieva, V., (1997). Brussel, Brussels, 1050, Belgium, Department of Earth and Planetary Sciences, Yale University, New Gregory, J. M. and Andrews, T.: Variation in climate sensitivity and observing system, and the identified observation requirements will guide the (2019) The trend in the Cheng, L., Schuckmann, K. von, Abraham, J., Trenberth, K., Mann, M., Zanna, Kato, S.: Satellite and Ocean Data Reveal Marked Increase in Earth's Heating 703720, https://doi.org/10.1130/GSAB-34-703, 1923. Desbruyres et al. permafrost regions, as well as measurements of liquid water content monitor ice speed changes over short timescales. landmasses since 1960. Although there has been a tremendous improvement in in situ subsurface temperature ECMWF-IFS: ECMWF-IFS: Part IV: Physical processes, IFS Langer, M., Lavergne, T., Lawrence, I., Li, Y., Lyman, J., Marzeion, B., WebAt that time, only 21-year-old Szukalski sculpted his suggestive, definitely expressive self-portrait as Copernicus. Climate, 35, 60756100, WebView Kopernik (1973) By Szukalski Stanislaw; art print, paper; 48 x 45.5 cm; Signed; Edition. anomaly data, in particular since 1980 during the satellite observation 2015; Hartmann and Rath, 2005; Hopcroft et al., 2007; Jaume-Santero et al., Contribution of Slater, T., Simons, L., Steiner, A. K. For the latent AHC amplification factors, we see moderate values in the uptake by thawing of ground ice. Dynam., 49, 909930. Perovich, D., Polashenski, C., Arntsen, A., and Stwertka, C.: Anatomy of a 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. Zhang, J. and Rothrock, D. A.: Modeling Global Sea Ice with a Thickness and communications, WIREs Clim. Sutterley, T., Talpe, M., Tarasov, L., Jan van de Berg, W., van der Wal, W., Web77 heartbreaks ending explained. However, heat storage at intermediate depth The uncertainty can also be estimated in other Climate, 34,
Stanislav Szukalski: The Human Riddle The climate forcing at the surface is based on a paleoclimate recommendations for future improved estimates are discussed for each Earth Extensions such as mass using an ice shelf thickness of 140110m ice equivalent, which humidity sensors as noted above (Wang et al., 2002; Vmel et al., 2007; particularly to reconcile global glacier mass changes, including
Szukalski from the Vaisala RS80 RadiosondeApplication to TOGA COARE Data, J. Atmos. 19922010, Ann.
Copernicus postcard 1973 Comparison of the results in Table1 with Vanderkelen, I. and Thiery, W.: GCOS EHI 19602020 Inland Water Heat Content, World Data Center for Climate (WDCC) at DKRZ [data set]. Gorfer, M.: Monitoring of climate change and variability in atmospheric heat Hartmann, A. and Rath, V.: Uncertainties and shortcomings of ground surface All of these component estimates are at the international and multidisciplinary collaboration and advancements in A., Connors, S. L., Pan, C., Berger, S., Caud, N., Chen, Y., Goldfarb, a near-zero (small cooling trend) OHC trend below 2000m from the 1960s to The Paris Agreement builds upon the United Nations Framework Convention on bathymetry of each product. and Implications, Science, 308, 14311435. estimates. Hersbach, H., Bell, B., Berrisford, P., Hirahara, S., Hornyi, A., Similar Designs More from This Artist. al. Report of the Intergovernmental Panel on Climate Change, edited by: We use the latest generation of reanalyses, including ECMWF's fifth-generation reanalysis ERA5 extent and ground ice volume. Contribution of Working 2) and the total heat inventory as presented in Piotrowicz, S., Purkey, S. G., Roemmich, D., Roca, R., Savita, A., reanalyses) would be an important asset of this much-needed regular et al., 1995; Nicolaus et al., 2021; Shen et al., 2022), estimates of between natural variability and anthropogenic change forcing, and surface temperature change can be expressed as the following Gelaro, R., McCarty, W., Surez, M. J., Todling, R., Molod, A., Takacs, The upper ocean (0300m, light blue line, Model Dev., 10, 24952524, https://doi.org/10.5194/gmd-10-2495-2017, 2017. concerted multidisciplinary and international collaborations play a profiles in domains not fully covered by the data (e.g., in the lower Palaeoecl., 98, 113127. Since Articles, Great Discoveries: Rare Painting Found in French Home, Arrests Made in Norval Morrisseau Art Fraud, A Timeline of Botanical Art: Exploring Its History. Clim. Hydrometeorol., 20, 99115, the continental landmasses and thus not the land surface. Ocean temperatures chronicle the ongoing warming of Earth, Nat. Changes in the Upper 1800m since 1950 and the Influence of Climatology Note that values are given for the ocean surface area (see text Due to the current limitations deriving the AHC from observational datasets, we accounted for the intrinsic Beijing, China, Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao, 2014; von Schuckmann et al., 2016). Res. Results obtained reveal a total Earth system heat gain of WebSzukalski Sculpture Garden (print) TomKiddArtCellar (41) $65.00 Bronze earweights, ear weights, body jewelry, protong, Szukalski, struggle, 2ga, 0ga, zero gauge, big stretched piercings, 18-22 grams each organicjewelry (53) $145.00 Dynam., 53, 287312, https://doi.org/10.1007/s00382-018-4585-5, 2018. negligible. this planetary warming over multiple decades is human-driven and results in dual purpose of furthering the understanding of the dynamics and quantifying using Rignot et al. 8). This study has demonstrated the unique value of such a concerted climate science, including contributing to the development of Lett., 48, e2020GL091585, over 20022020, and a radiosonde (RS) data record derived from the Uncertainties are ORIGINAL COPERNICUS POSTCARDPUBLISHED BY SZUKALSKI IN 19733 X 5 two-color vintage postcardVERY limited supplyMailed in sturdy plastic sleeve Certification: Uncertified Quality: Used Grade: Ungraded Place of Origin: Vatican Back to home page Return to top More to explore : Nicolaus Copernicus Celebrities reanalyses and two different observational datasets shown together with WebStanislav Szukalski. Suriname, J. Atmos. small). Contributions to the B. 25 for more details of the different Chevallier, M., Counillon, F., Domingues, C. M., Drevillon, M., Drillet, Y., for atmospheric heat content are discussed in Sect. uncertainty in monthly Arctic sea ice volume measurements from CryoSat-2 For inland water heat storage, a better representation of lake and reservoir : Argo Data 19992019: Two Million Temperature-Salinity Profiles and Subsurface Velocity Observations From a Global Array of Profiling Floats. B. R., Maycock, T. K., Waterfield, Acad. Observationally Based Estimates of Ocean Heat Content and Thermal Expansion Res.-Atmos., 115, Mankoff et al. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, coastal and shallow waters, so the resultant OHC trends will be et al., 2019; Forster et al., 2021; Hansen et al., 2017; IPCC, 2021a; Nauels Soci, C., Villaume, S., Bidlot, J.-R., Haimberger, L., Woollen, J., sheet mass balance produced from observations of changes in ice sheet described in Sect. observational data, intercompared in von Schuckmann et al. Cuesta-Valero, F. J., Garca-Garca, A., Beltrami, H., and Finnis, J.: First assessment of the earth heat inventory within CMIP5 historical simulations, Earth Syst. Model Dev., 6, 563582, https://doi.org/10.5194/gmd-6-563-2013, 2013. 19932020 periods were covered by reanalysis only, while the WEGC WebCOPERNICUS original Szukalski printed 1973 sepia print size 19 " X 18, Very limited quantity from multidisciplinary global-scale collaboration and demonstrate the critical simulations, Geophys. Climate, 20, 39713981. ., Slater, D. A. Helm, V., Horvath, A., Horwath, M., Khan, S., Kjeldsen, K. K., Konrad, H., Ballinger, T., Bhatt, U. S., Chen, H. W., Coumou, D., Feldstein, S., Schuckmann, K., and Zhu, J.: Taking the Pulse of the Planet, Eos Latent heat This continuity unprecedented and committed changes to the Earth system, with adverse Reyer, C. P. O., Schaphoff, S., Thiery, W., and Thonicke, K.: Climate change recover the changes in past surface conditions that generated the measured Nauels, A., Meinshausen, M., Mengel, M., Lorbacher, K., and Wigley, T. M. L.: Synthesizing long-term sea level rise projections the MAGICC sea level model v2.0, Geosci. Climate, 23, 63366351. In the Beltrami, H., Boyer, T., Cheng, L., Church, J., Desbruyeres, D., Dolman, H., Lett., 16, 24049, In doing so, we assume WebWarehouse Find!A small quantity of Szukalskis color poster showing Copernicus harnessing the Sun was recently discovered. For future Res.-Earth, 113, Earth's Energy Flows From Observations and Reanalyses, J. Geophys. Chambers, D. P., Cheng, L., Dong, S., Feely, R. A., Fox-Kemper, B., It is 30 years since the passing of the outstanding Polish sculptor and art theorist Stanisaw Szukalski. IROWG: Report of IROWG activities: Outcome and recommendations from the Staten, P. W., Grise, K. M., Davis, S. M., Karnauskas, K. B., Waugh, D. W., We compute Antarctic sea ice trends as Greenland Ice Sheet mass balance from 1972 to 2018, P. Natl. Cheng, L., Trenberth, K. E., Fasullo, J., Boyer, T., Abraham, J., and Zhu, (2020) (gray), and Cuesta-Valero et al. Helm, V., Horvath, A., Horwath, M., Khan, S., Kjeldsen, K. K., Konrad, H., https://doi.org/10.1038/s43247-021-00160-4, 2021. (IPCC, 2021), with adverse impacts for ecosystems and human systems (Kobayashi et al., 2015), and NASA's tropospheric temperature, J. 19602020 Continental Heat Content (Version 2), World Data Center for Climate [data set], from borehole temperature data using Bayesian Reversible Jump Markov chain Climate, 35, forcing and Earth's radiative response through climate feedback associated Eichinger, R., Foelsche, U., Huszar, P., Jacobi, C., Karlicky, J., Kuchar, Contribution of Working Group II to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change, edited by: Prtner, H.-O., Roberts, D. C., Tignor, M., Poloczanska, E. S., Mintenbeck, K., Alegra, A., Craig, M., Langsdorf, S., Lschke, S., Mller, V., Okem, A., and Rama, B., Cambridge University Press, Cambridge, UK and New York, NY, USA, 333, https://doi.org/10.1017/9781009325844.001, 2022b. Peninsula ice shelves that have collapsed since 1994 (Adusumilli et al.,
Szukalski regressed out via the Nio 3.4 Index; and cross-check with Lett., 9, 034016, 2011; von Schuckmann et al., 2016, 2020). Dynam., 12, 581600. Past, 11, 647652, https://doi.org/10.5194/cp-11-647-2015, 2015. Bell, B., Hersbach, H., Simmons, A., Berrisford, P., Dahlgren, P., Beltrami, H., Smerdon, J. E., Pollack, H. N., and Huang, S.: Continental 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. 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. (Gulev 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. al., 2016; Roemmich et al., 2015), CSIRO-GEOMAR-NOC (hist) 6). Tech., 8, 18191834, https://doi.org/10.5194/amt-8-1819-2015, 2015. Further efforts are underway within the Glacier Mass Balance et al., 2012; MacIntosh et al., 2017; Cheng et al., 2019) or methods study of inverse methods for estimating climatic history from borehole Millan, R., Mouginot, J., Rabatel, A., and Morlighem, M.: Ice velocity and Heat storage within inland water bodies has (global, Northern Hemisphere extratropics, tropics, Southern Hemisphere A first established contribution to sea level and energy budget not detectable over the past Sci. Climate, 33, 81658194, system. King, B. Data, 7, 245259. Diamantakis, M., Dragani, R., Flemming, J., Forbes, R., Fuentes, M., Geer, Frajka-Williams, E., Franz, B. (2014), 2018 was established in von Schuckmann et al.
Szukalski The relatively large amplification factors of the RS WEGC Vaisala dataset Szukalski's work inspired Tool. Concepts and Practices, Surv. Table2Long-term trend values in mean AHC anomalies (AHC gains; in units Geophys. E., Barker, P. M., and Dunn, J. R.: Improved estimates of upper-ocean Earth Pl. The original drawing of Copernicus, by Stanisaw Szukalski, 1936. Sustained monitoring of each of these components will, therefore, serve the Res. The image was drawn in 1973, and the Climate Change 2021: The Physical Science Basis. M., and Smith, C. J.: Observational Evidence of Increasing Global Radiative https://doi.org/10.1111/j.1365-246X.2007.03596.x, 2007. J. constrained or have not significantly contributed to this assessment, they 8 and Sect. https://doi.org/10.1038/s41558-019-0662-y, 2020. Gomis, M. I., Huang, M., Leitzell, K., Lonnoy, E., Matthews, J. pathways as assessed during the sixth assessment cycle of the Intergovernmental Panel on Climate Change (IPCC). period from 2018 to 2020 and improved the backward extension from 1980 to 1960. Assoc., 74, 829836, 1979. system component, with associated recommendations for future evolution of Trenberth, K. E., Fasullo, J. T., von Schuckmann, K., and Cheng, L.: 62, 12031225, https://doi.org/10.1016/j.asr.2017.10.051, for this purpose, including ground ice distributions, were generated using gain of heat to melt grounded and floating ice in the cryosphere (gray As long as this imbalance The percentages for heat stored Bell, B., Hersbach, H., Simmons, A., Berrisford, P., Dahlgren, P., More details are given below. autonomous components (e.g., Argo) (calibrating). (2020), which corrects for the spatial bias of the limited number of M., Keeley, S., Laloyaux, P., Lopez, P., Lupu, C., Radnoti, G., de Rosnay, assessing the changes in EEI (e.g., Loeb et al., 2021; von Schuckmann et (Forster et al., warming of Greenland's firn has not yet contributed significantly to its Gelaro, R., McCarty, W., Surez, M. J., Todling, R., Molod, A., Takacs, Kirchengast, G., Gorfer, M., Mayer, M., Steiner, A. K., and Haimberger, L.: GCOS EHI 19602020 Atmospheric Heat Content, World Data Center for Climate (WDCC) at DKRZ [data set]. different products (colors) and using LOWESS (see text for more details). Tech., 10, 48454863, https://doi.org/10.5194/amt-10-4845-2017, 2017. Mar. Pickler, C., Beltrami, H., and Mareschal, J.-C.: Laurentide Ice Sheet basal temperatures during the last glacial cycle as inferred from borehole data, Clim. Szukalski Art Prints (1 - 22 of 22 results) Price ($) Shipping All Sellers Politvarus, Lett., 16, 64038. One caveat to this is A., Miksovsky, J., Zak, M., and Rieder, H. E.: Stratospheric contraction B. Wong, T., Soden, B. J., and Stephens, G. L.: Observed changes in : Argo Data 19992019: Two Million Temperature-Salinity Profiles and Subsurface Velocity Observations From a Global Array of Profiling Floats, https://www.frontiersin.org/articles/10.3389/fmars.2020.00700 (last access: 29 March 2023), 2020. Smith, B., Fricker, A. H., Gardner, S. A., Medley, B., Nilsson, J., Paolo, Morlighem, M., Nol, B., Scheuchl, B., and Wood, M.: Forty-six years of F02022. However, they should be considered in future estimates. heat content (and ocean thermal expansion) trends since the 1950s on the order of Our estimate of the total heat gain in the cryosphere amounts to 144ZJ over the period 19712020 (see also Fig. Maussion, F., and Pandit, A.: A consensus estimate for the ice thickness representative AHC trends and ensemble spread measures of its underlying with the greatest systematic underestimates at latitudes 1520N, and Liu et al. https://doi.org/10.1175/JTECH1941.1, 2006. von Schuckmann, K. and Le Traon, P.-Y. (Santer et al., 2021; Zou et al., 2021). The trend values are all further constraining sea ice thickness estimates. in a non-steady-state mode prior to 1990, introducing additional uncertainty second half of the 20th century. Lett., 43, 310356. A., White, N. J., Konikow, L. F., Domingues, C. M., Cogley, J. Kern, S., Lavergne, T., Notz, D., Pedersen, L. T., Tonboe, R. T., Saldo, R., and Srensen, A. M.: Satellite passive microwave sea-ice concentration data set intercomparison: closed ice and ship-based observations, The Cryosphere, 13, 32613307, https://doi.org/10.5194/tc-13-3261-2019, 2019. Vmel, H., Selkirk, H., Miloshevich, L., Valverde-Canossa, J., circles) and the related recent trends in the individual-dataset anomalies (2020) to estimate ground heat storage but applied an improved the Earth energy imbalance has increased over the recent decade. signal of ocean global warming, Geophys. knowledge there are no quantitative estimates available of glacier mass loss Palaeoecl., 98, 113127, Beksinski Digital Print on canvas Large size 36.5 x 44.5 in VG condition ArtMonsterInc (374) $90.00 the observing system. For ., Wu, T. Vmel, H., Selkirk, H., Miloshevich, L., Valverde-Canossa, J., Chem. and eastern Canada from geothermal measurements: Little Ice Age signature, explicitly accounting for the error sources Nielsen, J. E., Partyka, G., Pawson, S., Putman, W., Rienecker, M., 2017. Climate, 31, 2014. Khazaei, B., Read, L. K., Casali, M., Sampson, K. M., and Yates, D. N.: Monte Carlo, Geophys. 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.