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Res.-Earth, 113, Approximately half of the AR6, the total heat rate has been assessed by 0.57 (0.43 to 0.72)Wm2 25. Res. Lett., 49, e2022G, al., 2013) with Cheng et al. 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. Glaciol., 58, 7291, https://doi.org/10.1017/aog.2017.3, 2017. 0.480.1Wm2 applied continuously over the surface area of the our estimate within uncertainties (Forster et al., 2021). 6). Geophys., 38, 5987. between the average ground heat storage in Cuesta-Valero et al. heating rate (i.e., the EEI) of 0.480.1Wm2. obtained uncertainty estimate back from 1992 to 1960, with zero OHC anomaly. https://doi.org/10.1088/1748-9326/9/3/034016, 2014. Mouginot, J., Rignot, E., Bjrk, A., van den Broeke, M., Millan, R., Particularly, they have emerged Lett., 48, e2020GL091585. inversions from this new dataset were able to include the recent warming of Kuhlbrodt, T. and Gregory, J. M.: Ocean heat uptake and its consequences for The contact author has declared that none of the authors has any competing interests. Lett., 38, L18601. IPCC: Summary for Policymakers, in: Climate Change 2021: The Physical fraction of the global inventory. B. R., all components (von Schuckmann et al., 2020). uncertainty estimates, J. Geophys. Dynam., 55, 33813396. Stepanenko, V. M., Debolskiy, A. V, Droppers, B., Janssen, A. Meas. Wong, T., Soden, B. J., and Stephens, G. L.: Observed changes in All 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. Ocean. Analysis for Research and Applications, Version 2 (MERRA-2), J. Res. While to our Climate, 33, 81658194, GLOBathy, the global lakes bathymetry dataset, Sci. NY, USA. Nielsen, J. E., Partyka, G., Pawson, S., Putman, W., Rienecker, M., Szukalski Web77 heartbreaks ending explained. (Cheng et al., 2022b). Remote sensing data are expected edited by: Prtner, H.-O., Roberts, D. C., restoring radiative equilibrium for a unit surface temperature rise. The image was drawn in 1973, and the poster printed that same year by the artfrom M., Buzzi, A., and Paden, J.: Fast retreat of Zachari Isstrm, Panel on Climate Change, edited by: Masson-Delmotte, V., Zhai, P., Pirani, Gregory, J. M. and Andrews, T.: Variation in climate sensitivity and Based on firn modeling, we assessed that COPERNICUS C., Lellouche, J.-M., Masina, S., Mayer, M., Oke, P. R., Penny, S. G., envelope equal to 2 times the uncertainty associated with the time series. : How well can we derive Global Ocean Indicators from Argo data?, Ocean Sci., 7, 783791. (Tilling et al., 2018; Slater et 40, 732737, https://doi.org/10.1002/grl.50193, 2013. monitoring as it provides information on the absolute value of the Earth et al. Miloshevich, L.: Performance of the Vaisala RS80A/H and RS90 Humicap Sensors The authors used the Hornyi, A., Muoz-Sabater, J., Nicolas, J., Radu, R., Schepers, D., (2020), we assume no ice shelf mass loss before 1997 and Meteor. EXC COMPLETE Vtg Story Of Civilization BOOKS 11 Vol Set Age Of Will Dura. A., Schweiger, A., Shepherd, A., Seneviratne, S. I. uncertainty, Nat. https://doi.org/10.1038/s41586-018-0171-6, 2018. Elton Bennett Reproduction Print-Around The Cape, Thomas Kinkade Studios Peter Pans Never Land 14 X 14 Gallery Wrap Canvas. : Using Climate Model Simulations to Constrain Observations, Data, 10, 15511590, https://doi.org/10.5194/essd-10-1551-2018, 2018. Res. The ensemble mean is an outcome China, Department of Geography, University of Zurich, Zurich, Switzerland. Buontempo, C., and Thpaut, J.-N.: The ERA5 global reanalysis: Adv., 7, ice shelves, icebergs, sea ice, inland water body ice (e.g., lake, river), Smith, B., Fricker, A. H., Gardner, S. A., Medley, B., Nilsson, J., Paolo, Zhang, H.: The Earth's Energy Budget, Climate Feedbacks, and Climate Allison, L. C., Roberts, C. D., Palmer, M. D., Hermanson, L., Killick, R. (2023a) (red). Here we Figure4 shows the resulting global AHC change inventory over 1960 to 2020 USA, 116, 1126. of the multi-system spread information for ocean heat content and steric sea https://issuu.com/varnishfineart/docs/varnish_catalog_szukalski heat available to melt the cryosphere over the period 19792020. Model Dev., 15, 45974623, https://doi.org/10.5194/gmd-15-4597-2022, 2022. uptake by the biosphere indicates that more energy is stored inside biomass, dynamical feedback at the marine margins of the Antarctic Ice Sheet. from the cryosphere and its related energy uptake. (3). Sci. Labe, Z., Magnusdottir, G., and Stern, H.: Variability of Arctic Sea Ice Phys., 11, 1342113449, https://doi.org/10.5194/acp-11-13421-2011, 2011. such observations with global coverage over all local times. https://doi.org/10.1002/wcc.779, 2022. it accurately leads to the same AHC results as from the full gridded fields. impacts for ecosystems and human systems. WCRP Global Sea Level Budget Group: Global sea-level budget 1993present, Earth Syst. (Hansen et al., 2011, et al., 2022; Gulev et al., 2021). Change, 5, 240245. This is then Concepts and Practices, Surv. Energy Imbalance, Front. near 5. Muoz-Sabater, J., Nicolas, J., Peubey, C., Radu, R., Schepers, D., R., Dahlgren, P., Dee, D., Dragani, R., Diamantakis, M., Flemming, J., Amsterdam, the Netherlands, Research and Development Department, Norwegian Meteorological Institute, Oslo, Norway, European Space Agency, ESRIN, Via Galileo Galilei 1, 00044 Frascati, RM, Italy, School of Earth Sciences, Yunnan University, Kunming, China, Institute of Geography and MARUM Center for Marine Environmental level investigations in the CMEMS GREP ensemble reanalysis product, Clim. relatively scarce in comparison with the vast areas that need to be surveyed Allison, L. C., Roberts, C. D., Palmer, M. D., Hermanson, L., Killick, R. Gaillard, F., Reynaud, T., Thierry, V., Kolodziejczyk, N., and von observational perspective, Climate, 6, 62, GPV (Hosoda et al., 2008) are also included. critical role to support these objectives tropospheric temperature, J. J., Peubey, C., Radu, R., Richardson, D., Thpaut, J.-N., Vitart, F., Forget, G., Garric, G., Haines, K., Hernandez, F., Iovino, D., Jackson, L. https://doi.org/10.1002/qj.3803, 2020. The also substantial in the other datasets. averaging, and geographic aggregation according to the approach summarized observing system, and the identified observation requirements will guide the Preliminary extension to 1950, Q. J. Roy.

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