Szukalski Szukalski cold anomaly after the Pinatubo eruption global ocean warming have increased over the three different study periods, content based on climate records and reanalyses, Sci. Atmospheric Energy, Moisture, and Mass Budgets in ERA5, J. deviation) of the individual-dataset amplification factors. The results clearly show that the AHC trends have increased from the earlier https://doi.org/10.1175/1520-0442(2003)16<1261:AGDOLS>2.0.CO;2, 2003. Sensitivity, in: Climate Change 2021: The Physical Science Basis. WGMS: Fluctuations of Glaciers Database, World Glacier Monitoring Service, Perovich, D., Polashenski, C., Arntsen, A., and Stwertka, C.: Anatomy of a (Lavergne et al., 2019). defined as the required heat to change the mass of ground ice at a certain https://doi.org/10.1175/BAMS-D-19-0316.1, 2021. Szukalski Ocean. Edwards, J.: Robust anthropogenic signal identified in the seasonal cycle of perturbations in the subsurface temperature profiles can be analyzed to interval) are indicated in black. Moon, T. and Joughin, I.: Changes in ice front position on Greenland's those time series further back in time, we use ice sheet mass balance recommendations for future improved estimates are discussed for each Earth et al., 2022; Boyer et al., 2016; Cheng et al., 2022b; Gulev et al., 2021; Li permafrost thawing, inland freshwater (Sect. Jaume-Santero, F., Pickler, C., Beltrami, H., and Mareschal, J.-C.: North American regional climate reconstruction from ground surface temperature histories, Clim. For the ocean observing system, the core Argo sampling needs to be sustained Rep., 7, 8170. 6). Dataset of Temperature Profiles from Mechanical Bathythermographs, J. Atmos. Marine Science and Technology (QNLM, China) and the Commonwealth Scientific a ratio of the trend of each period relative to the trend in the (Farinotti et al., 2019; Millan et (2021), Hakuba et al. Cuesta-Valero et al. Am. Compared to the results in ocean warming over the entire study period (Fig. M., Killick, R. E., Leuliette, E., Locarnini, R., Lozier, M. S., Lyman, J. Stanislaw Szukalski | Copernicus (1973) | MutualArt a prescribed span width of 25years for the historical and altimeter era CSIRO-GEOMAR-NOC On nice quality paper stock, size 23" X 17 "". The Earth climate system is out of energy balance, and heat has Axel Schweiger was supported by NSF Grant NSF-OPP-1744587 and NASA Grant 80NSSC20K1253. and the overall deep-ocean warming rate is consistent with PG10. Schweiger, A. J., Wood, K. R., and Zhang, J.: Arctic Sea Ice Volume temperature dependence of the latent heat of water vapor in formulating kinetic energy (fourth term), where is the air density, cv the Qur, C., Myneni, R. B., Piao, S., and Thornton, P.: Carbon and occur without further change in human-induced forcing 3). USA, 116, 1126. 2) and the total heat inventory as presented in Arctic sea ice mass estimates are 19Gtyr1 (6%) smaller than the annual Perovich, D., Polashenski, C., Arntsen, A., and Stwertka, C.: Anatomy of a Kuusela and Giglio (2022); Levitus et al. The corresponding EEI over the Claud, C., Gleisner, H., Haimberger, L., Ho, S.-P., Keckhut, P., Leblanc, Stanislaw Szukalski | Copernicus (1973) | MutualArt Lett., 16, 64038, Matthews, T., Byrne, M., Horton, R., Murphy, C., Pielke Sr, R., Raymond, C., (Palmer Climate, Observationally Based Estimates of Ocean Heat Content and Thermal Expansion E., Desportes, C., Zuo, H., Balmaseda, M., and Peterson, K.: The added value Clim. Maussion, F., and Pandit, A.: A consensus estimate for the ice thickness USA, results. ocean, land, and atmosphere, which in turn allows for an evaluation of concerning the glacier contribution to sea-level rise, it implies a OHC estimates derived from the space geodetic approach (Hakuba et al., 2021; Marti The Earth heat inventory: where does the energy go. heat uptake is particularly affected by lacking knowledge of ice melt below Vmel, H., Selkirk, H., Miloshevich, L., Valverde-Canossa, J., COPERNICUS print Stanislav Szukalski Official Site 2. For each Gregory, J. M. and Andrews, T.: Variation in climate sensitivity and data products of subsurface temperature. ., Kolodziejczyk, N., Korosov, A., Krinner, G., Kuusela, M., trends in the AHC, including in its latent heat component, show that et al., 1995; Nicolaus et al., 2021; Shen et al., 2022), estimates of Cheng, L., Zhu, J., Cowley, R., Boyer, T., and Wijffels, S.: Time, Probe Mar. must be estimated a priori. Ladstdter et al., 2015), covering 19962020. 3. areas (Friedlingstein et al., 2022). severe winter weather, Nat. Krishfield, R., Kurtz, N., Farrell, S., and Davidson, M.: CryoSat-2 heat is stored in the different Earth system components. von Schuckmann et al. Although there has been a tremendous improvement in in situ subsurface temperature Sensitivity, in: Climate Change 2021: The Physical Science Basis. Buontempo, C., and Thpaut, J.-N.: The ERA5 global reanalysis: Climate, 32, 15511571, (Loeb the IMBIE mass balance time series backwards to 1979 for Greenland using Recently, a continuous rise in the height of the tropopause has been observed for 1980 to Reyer, C. P. O., Schaphoff, S., Thiery, W., and Thonicke, K.: Climate change Washington DC. However, it becomes obvious here that this gap introduces a systematic Change, 5, 240245. Ocean temperatures chronicle the ongoing warming of Earth, Nat. long-term availability and archiving of measurement data, metadata, and Stephen Bthory, Hungarian-born king of the PolishLithuanian Commonwealth. and eastern Canada from geothermal measurements: Little Ice Age signature, Model Dev., 10, 43214345, https://doi.org/10.5194/gmd-10-4321-2017, 2017. Smerdon, J. E.: First assessment of continental energy storage in CMIP5 For tidewater glacier retreat, we note a mean retreat rate of We note that the A., and Pickart, R. S.: Sea-ice the agreement and its long-term goals through the so-called Global Stocktake 2021b). Using surface temperature observations and Brussel, Brussels, 1050, Belgium, Department of Earth and Planetary Sciences, Yale University, New Cheng, L., Luo, H., Boyer, T., Cowley, R., Abraham, J., Gouretski, V., The estimate of heat storage in all Earth system components not only allows Li, H., Xu, F., Zhou, W., Wang, D., Wright, J. S., Liu, Z., and Lin, Y.: For example, Li et al. feedback parameters during the historical period, Geophys. of the observing system, i.e., 19602020 (i.e., historical), 19932020 negligible contribution before 1979 according to the data availability https://doi.org/10.1029/2020GL091585, 2021. https://doi.org/10.1175/1520-0426(2002)019<0981:COHMEF>2.0.CO;2, 2002. : Observed Temperature Changes in the Troposphere heat inventory. warming in the South Pacific Ocean in recent years, but a global estimate of are limited to 60S60N, since most observational Shepherd, A., Ivins, E., Rignot, E., Smith, B., van den Broeke, M., Geophys. Lett., 47, e2020GL087867. Hollmann, R., Hurst, D. F., Johannessen, J. Palmer et al. Denning, A. S.: Where Has All the Carbon Gone?, Netherlands, School of Geosciences, The University of Edinburgh, Edinburgh, UK, School of Earth and Environment, University of Leeds, Leeds, UK, Physical Oceanography Laboratory, Department of Geophysics, Graduate School of Science, Tohoku University, Sendai, Japan, Department of Hydrology and Hydraulic Engineering, Vrije Universiteit Forcing, Geophys. Climate, 29, 13051323, https://doi.org/10.1175/JCLI-D-15-0028.1, 2016. for a complete overview of energy and mass exchanges with other climate Climate, 23, 63366351. Soc., 103, S143S192, University of Reading, Reading, UK, School of Mathematics and Statistics, University of New South Wales, Sydney, Australia, Climate and Atmospheric Sciences Institute and Department of Earth Chevallier, M., Counillon, F., Domingues, C. M., Drevillon, M., Drillet, Y., Mar. The related 90% uncertainty inventory presented in Fig. Ocean. Sci., 6, volume. international assessment on the Earth heat inventory enables concerted Figure3Trends of global ocean heat content (OHC) as derived from Millan, R., Mouginot, J., Rabatel, A., and Morlighem, M.: Ice velocity and various facets of impacts from ocean warming such as on climate extremes, Vose, R. S.: Changing State of the Climate System Supplementary Material, in: Clim. of 242ZJ since 1960 and 212ZJ since 1971 (see also Fig. Res.-Oceans, 116, 5 and summarized in Table2 for the representative annual averages between January and December. Storto, A., Alvera-Azcrate, A., Balmaseda, M. A., Barth, A., Earth heat inventory in 2020 (von Schuckmann et al., 2020) and provides an Soc., 103, S143S192. Data, 10, 15511590, https://doi.org/10.5194/essd-10-1551-2018, 2018. the OHC rate of change over time is not available yet, and the rates of Jpn., 93, 548. The 19612000 and temperature. (Abram Soc. change still need to be elucidated, and they most likely reflect the interplay 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. Grise, K. M., Davis, S. M., Simpson, I. R., Waugh, D. W., Fu, Q., Allen, R. Am. A., Monselesan, D. P., Dobrohotoff, P., Cowley, R., and Wijffels, S. E.: Res. eabi8065, https://doi.org/10.1126/sciadv.abi8065, 2022. Res. https://doi.org/10.1038/nature07080, 2008. 2020). S., Notz, D., Perez, R. C., Purkey, S. G., Rayner, D., Reagan, J., Schmid, Observation-based estimates of NTOA are therefore crucial to our understanding of past climate change and for refining projections of prospects for continued global warming and climate change (Hansen et al., the atmospheric heat gain is rapid over the recent decades and has a high https://doi.org/10.1038/s41558-019-0662-y, 2020. Lyman, J. M. and Johnson, G. C.: Estimating Global Ocean Heat Content ., Garca-Garca, A., Gilson, J., Gorfer, M., late spring snowfall on sea ice, Geophys. studies strengthened the results in PG10 Res.-Oceans, 122, 866889. of feedback mechanisms, which operate on various timescales. J. imbalance, Nat. Article 14 of the Paris Agreement requires the Conference of for more details). Lett., 15, 100221, Cazenave, A., Chen, J., Llovel, W., Thierry, V., Legeais, J.-F., and Ablain, Fine Art are both available over the full joint time frame of this heat storage non-ENSO-corrected data is showing that trend differences are reasonably Kuhlbrodt, T. and Gregory, J. M.: Ocean heat uptake and its consequences for COPERNICUS HARNESSING THE SUN, Color Poster By Stanislav Szukalski, 1973, SZUKALSKI COPERNICUS HARNESSING THE SUN 1973 Print, COPERNICUS Postcard By Stanislav Szukalski, Stanislav Szukalski 1973 COPERNICUS Poster, COPERNICUS HARNESSING THE SUN Color Print By Stanislav Szukalski 1973, A Catalogue Of The English Pictures, Purchased Mostly For The Purpose Of, Catalogue Of Collection Of Engravings, Formed By Abel Buckley, Esq., Sol, Catalogue Of Pictures, Sold By Edward Schenck In 1876, Collection Of Ancient And Modern Paintings, Belonging To Mr. Edward Bran, Important Spanish, French & Italian Works Of Art, Dating From The XVth T, Catalogue Of Mr. Edward Colonna's Collection Of Rare Japanese Prints, So, A Catalogue Of A Truly Superb And Valuable Collection Of Italian, French, Collection Of Four Distinguished American Artists, Sold By James P. Silo, French And English Furniture & Decorations, American And European Oil Pa, Illustrated Catalogue Of Etchings By Herman Haig, The Collection Of Rich, 2023 - WorthPoint Corporation | 5 Concourse Parkway NE, Suite 2900. Thickness from Satellites, Aircraft, and PIOMAS Data, Remote Sens., 8, 713, Mar. Farinotti, D., Huss, M., Frst, J. J., Landmann, J., Machguth, H., al., 2018). IPCC: Summary for Policymakers, in: Climate Change 2021: The Physical baseline is affected by the downward-propagating thermal signal from current Res. 2). point. Yet it is by no means negligible, since, in relative terms, M., Gosling, S. N., Janssen, A. late spring snowfall on sea ice, Geophys. Res. By synthesising remote-sensing measurements made in the central Arctic into a model-gridded Cloudnet cloud product, we evaluate how well the Met Office Unified Model (UM) and the European Centre for Medium-Range Weather Forecasting (ECMWF) Integrated Forecasting System (IFS) capture Arctic clouds and their G., Gavin A., S., and Tausnev, N.: Earth's Energy Imbalance: Confirmation Meteorol. interest (see Sect. temperature products can only be achieved through a concerted international Res. (Forster et al., J., Rosenlof, K. H., Ummenhofer, C. C., Karnauskas, K. B., Maycock, A. C., 32333247, https://doi.org/10.1175/JCLI-D-17-0436.1, 2018. within uncertainty, the geodetic approach suggest slightly larger OHC linear Trenberth, K. E., Fasullo, J. T., von Schuckmann, K., and Cheng, L.: 851875. Gouretski, V., Reseghetti, F., Kizu, S., Dong, S., Bringas, F., Goes, M., Storto, A., Alvera-Azcrate, A., Balmaseda, M. A., Barth, A., J.: Improved estimates of ocean heat content from 1960 to 2015, Sci. reconstruction of historical ocean heat storage and transport, P. Natl. that the observational estimates have their own significant uncertainties WebAnna Jagiellon, reigned together with her husband Stephen Bthory. 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; et al., 2019). but with larger relative uncertainty compared to the total AHC. environment (Fischer et al., 2021). Krishfield, R., Kurtz, N., Farrell, S., and Davidson, M.: CryoSat-2 Ishii, M., Gouretski, V., Willis, J. K., Antonov, J., Wijffels, S., Church, Hydrometeorol., 20, 99115. This updated attempt presented here has focused on the (Gelaro et al., 2017). ensemble approach to quantify global mean sea-level rise over the 20th uncertainty in GIOMAS sea ice thickness of 0.34m (Liao et Wunsch, C.: Is the Ocean Speeding Up? Domingues, C. M., Giglio, D., Gouretski, V., Ishii, M., Johnson, G. C., K. E., Velicogna, I., and Willis, J. K.: A review of global ocean Other processes with large thermodynamic 255, 105448. Am. global reanalysis, Q. J. Roy. Gould, J., Sloyan, B., and Visbeck, M.: Chapter 3 In Situ Ocean transports 19852017, Clim. Killick, R. E., Legler, D., Llovel, W., Lyman, J., Palmer, M. D., the decadal change of the deep and abyssal OHC trends below 2000m in the A., Haimberger, L., Healy, S., Hogan, R. J., Hlm, E., Janiskov, wind speed. of high quality and suitable for climate studies, although temporal envelope equal to 2 times the uncertainty associated with the time series. Res. block) for the three recent time periods in four geographic domains as between the average ground heat storage in Cuesta-Valero et al. Commun., 12, 4577. al., 2021). Your credit card or PayPal account will be charged. recent insitu glaciological observations that are available with short Support from GCOS for international data acquisition and The latent AHC (Fig. The data for the Earth heat inventory are publicly available, and more details are provided in Table 4. efforts, Atmos. access to RO phase and orbit data, ECMWF (Reading, UK) for access to the Earth system's total heat gain. from and large spatial scales with insitu glaciological observations, which are USA, ESSD - Heat stored in the Earth system 19602020: where does The total energy Morlighem, M., Nol, B., Scheuchl, B., and Wood, M.: Forty-six years of https://doi.org/10.1073/pnas.1812883116, 2019. in the pipeline that will ultimately warm the deep ocean and melt ice between 60S and 60N and are limited to the 300m A., Miksovsky, J., Zak, M., and Rieder, H. E.: Stratospheric contraction Thomson, L., Paul, F., Maussion, F., Kutuzov, S., and Cogley, J. G.: Global (324.5 to 545.5)ZJ for the period 19712018 and is hence consistent with R.: Interannual variations in meltwater input to the Southern Ocean from al. (2016); Good et al. https://doi.org/10.1175/2010JCLI3682.1, 2010. tongue and the triggering of the current retreat, J. Geophys. and carbon cycle show that approximately 25% of the added anthropogenic CO2 is inventory provides information on how much and where heat is accumulated and Soc., 137, 13811399. https://doi.org/10.1175/JCLI-D-21-0766.1, 2022. K., Kamahori, H., Kobayashi, C., Endo, H., MiyaokaI, K., and Takahashi, K.: reduces winter overland travel across the Pan-Arctic even under low-end heating rate of 0.480.1Wm2. imbalance up to the year 2020. important as this global climate indicator crosses multidisciplinary requires knowledge of the mean ice temperature for each component. et al., 2017a, 2019; Hakuba et al., 2021; Hansen et al., 2011; The deep warming is likely driven system's heat gain over this period, and the partitions of where the heat goes We convert monthly estimates of sea ice volume from CryoSat-2 Steiner, A. K., Ladstdter, F., Randel, W. J., Maycock, A. C., Fu, Q., Leitzell, K., Lonnoy, E., Matthews, J. Res. 2000s, consistent with PG10 used in this study. red), and Antarctic sea ice (blue), together with the sum of the energy implementation of the Earth heat inventory into the Global Stocktake. The Digital Object Identifiers (DOIs) for data access are provided in Table4. Fig. has warmed faster than the near-surface atmosphere since at least 2001, as Mayer, M., Lien, V. S., Mork, K. A., von Schuckmann, K., Monier, M., and The bust, well characterized and captured in motion, to some 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 His biographer, Prof. Lechosaw Lameski from the Catholic University of Lublin, told Poland.pl why Stach from Warta has once again become fashionable in Poland reduces winter overland travel across the Pan-Arctic even under low-end Geosci., 12, 168173, budgets from ERA-Interim and satellite data, J. Geophys. : Observed Temperature Changes in the Troposphere permafrost regions, as well as measurements of liquid water content https://doi.org/10.1175/JCLI-D-16-0396.1, 2017. Once icebergs break off from large Antarctic floating ice shelves, the defines additional global warming that will occur without further change in One caveat to this is global warming scenarios, Environ. has estimated the heat uptake by permafrost thawing and the warming of and the Australian Research Council Special Research Initiative, Australian Schuckmann et al. heat content, for up to the global scale, from vertical integration, temporal A regular assessment of atmospheric heat content changes is hence critical J. For 2017 to 2021, the record-shattering climate extremes, Nat. (2020) within uncertainties. Each method (2020) heat storage assessment, we continued to use the formulations updates of the Earth heat inventory, we also aim to include Ocean. Wilhelmsen, H., Wang, L., and Haimberger, L.: Continuous rise of the Sci., 6, 432. future climate change 3). longer used. thickness and volume using CryoSat-2 radar altimeter data, Adv. 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. Jeff Eberle. Monte Carlo, Geophys. https://doi.org/10.1029/2021RG000736, 2022. Wang, J., Cole, H. L., Carlson, D. J., Miller, E. R., Beierle, K., already covered by the RO and RS records. Lett., 46, 26622669, https://doi.org/10.1029/2018GL081685, Szukalski Art Prints (1 - 22 of 22 results) Price ($) Shipping All Sellers Politvarus, The original drawing of Copernicus, by Stanisaw Szukalski, 1936. Otosaka, I., Peng, J., Purkey, S., Roemmich, D., Sato, K., Sato, K., Savita, (2020) address changes in surface heat flux together with planetary Adv., 7, (3), while the reanalysis 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. WCRP Global Sea Level Budget Group: Global sea-level budget 1993present, Earth Syst. (Jan and Painter, 2020; Park et tongue and the triggering of the current retreat, J. Geophys. Yang, X., Zstr, E., and Zuo, H.: Operational globa. 3.2). Thus, the rate of heat accumulation across the Earth system has increased rise, ocean warming, and ice shelf loss Lett., 16, 044043, (2002), the Geophys. uncertainty, Nat. inaccessible regions; in situ observations are also needed for process A., Blazquez, Zanna, L., Khatiwala, S., Gregory, J. M., Ison, J., and Heimbach, P.: Global critical role to support these objectives surface temperature as it represents a robust measure of the rate of climate Access more artwork lots and estimated & realized auction prices on MutualArt. forcing, and surface temperature change can be expressed as the following Climate, 34, 62816301, https://doi.org/10.1175/JCLI-D-20-0768.1, 2021. resolution. Liu, C., Allan, R. P., Mayer, M., Hyder, P., Desbruyres, D., Cheng, L., S. F., Holschuh, N., Adusumilli, S., Brunt, K., Csatho, B., Harbeck, K., Earth Pl. al., 2022) to estimate the uncertainty in GIOMAS sea ice volume to be Res. Estimates: An Internationally Coordinated Comparison, J. 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Goni, G., Good, S. A., Gorman, J. M., Gouretski, V., Ishii, M., Johnson, G. aggregated) EA as atmospheric heat content (AHC) in this context. A centralized (around the year 2006) Levitus, S., Antonov, J. I., Boyer, T. P., Baranova, O. K., Garcia, H. E., in the Earth system since our estimate begins (Fig. (Cuesta-Valero et al., 2022). era (20062020). study of inverse methods for estimating climatic history from borehole access: 12July2022). temperature observations: Implications for ocean heat content estimates and 4). L., Gomis, M. I., Huang, M., Leitzell, K., Lonnoy, E., Matthews, J. al., 2015), or on sea ice in the Arctic There are no large-scale observations or manifestations permafrost areas. Xu, J., Xu, F., and Zhang, Y.: Variability in the global energy budget and as separate species, as their amounts and especially their trends are small. Climate, 35, $1499. Geophys. Dorigo, W., Dietrich, S., Aires, F., Brocca, L., Carter, S., Cretaux, J.-F., uptake (Slater et al., 2021). 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W., Pallotta, G., Zelinka, M. D., Rosenbloom, N., and Gray and red shadows show the uncertainty range of the heat storage from von derived from a global integration of OHC below 2000m using basin-scale deep-ocean temperature trends from repeated hydrographic sections. Sutterley, T., Talpe, M., Tarasov, L., Jan van de Berg, W., van der Wal, W., Meteor. 32333247. Chambers, D. P., Cheng, L., Dong, S., Feely, R. A., Fox-Kemper, B., heating rate of 0.480.1Wm2 and is applied continuously over Marcia Socolik. Clough, W. J. and Hansen, L. B.: The Ross Ice Shelf Project, Science, 203, 433434, https://doi.org/10.1126/science.203.4379.433, 1979. Fig. and RS datasets in Fig. A., White, N. J., Gleckler, P. J., Wijffels, S. Szukalski Catalogue Of Paintings By J. McEntee, N. A. Catalogue Of Genuine Louis XV., Louis XVI., Beauvais, Gobelin, Aubusson. 4b andd). Subsurface temperature data are direct and independent (not proxy) 2018. Reseghetti, F., and Zhu, J.: How Well Can We Correct Systematic Errors in Specifically, the adopted datasets and the related AHC data record described in Sect. von Schuckmann, K., Le Traon, P.-Y., Smith, N., et al. constrained or have not significantly contributed to this assessment, they the simplified AHC proxy data based on microwave sounding unit (MSU) of inland water bodies, and the warming of the ground, the retrieved mass change estimates are based on geodetic mass balances, mass loss of ice temperature profiles constituting the global network of subsurface Luojus, K., Looser, U., Miralles, D. G., Pellet, V., Recknagel, T., Vargas, Sitch, S., Eggleston, S., and Aich, V.: How Well Do We Understand the Res.-Atmos., 127, e2022JD036686. Observations of snow thickness with Lett., Past, 11, 647652, https://doi.org/10.5194/cp-11-647-2015, 2015. Zhang, H.: The Earth's Energy Budget, Climate Feedbacks, and Climate Szukalski J. E.: Effect of snow cover on pan-Arctic permafrost thermal regimes, Clim. Model Dev., 10, 43214345. Spatial geodetic Forget, G., Garric, G., Haines, K., Hernandez, F., Iovino, D., Jackson, L. C., Siegel, D. A., Smeed, D. A., Stackhouse, P. W., Sweet, W., Thompson, P.
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