Fig. 1 AMOC stability in modern climate and AMOC response under global warming. AMOC stability in modern climate and AMOC response under global warming.

Slides:



Advertisements
Similar presentations
© red ©
Advertisements

Is this a square or a pentagon? It is a square.
If you say 8 color the ones in your picture purple. If you say 9 color the ones in your picture blue.
Colors.
Like.
Empirical mutation-selection phase diagram of tumor evolution.
Name: _______________________________
Average Number of Photons
Warm up create a step and leaf plot based on the data below

Can I color yellow?. Can I color yellow?
How Many Colorful Shapes?
Volume 111, Issue 2, Pages (July 2016)
What Color is it?.
©
C c Cc is for cat. © ©
©
Plots of the number of sequences [log (x + 1) scale] from bacterial OTUs in both PCR replicates (PCR1 and PCR2) of the 348 wild rodents analyzed in the.
by Wei-Ping Chan, I-Ching Chen, Robert K
Evolution of the global surface temperature of the last 22 ka: the reconstructions of M13 (1) (blue) after 11.3 ka and by Shakun et al. Evolution of the.
Correlations between metabolic pathway abundances and environmental conditions deduced from the ocean samples in this study, at various levels of model.
Help Gina and Tina color the numbers
Linked canopy, climate, and faunal change in the Cenozoic of Patagonia
Shapes.
Color Box Button - Gray Type : object Type : object Type : object
Fig. 1 Upward emission functions used to compute the maps.
Fig. 2 Tera-Wasserburg plot of zircon dates from LASS and APM data.
Fig. 1 Overall structure and organization of the major and minor capsid proteins in HAdV-D26. Overall structure and organization of the major and minor.
Fig. 4 Estimations of nonlinear functionals of a single-qubit state with the quantum Fredkin gate. Estimations of nonlinear functionals of a single-qubit.
Fig. 4 States of the Antarctic Ice Sheet after 10,000 years.
Fig. 5 Time evolution results of the MIROC climate model simulation with freshwater hosing. Time evolution results of the MIROC climate model simulation.
Fig. 2 Box plots of water use with lateral lengths.
Fig. 1 Evolution of magnetic field lines around a foreshock bubble in the GSE-XY plane (z = 0): Results of a hybrid simulation. Evolution of magnetic field.
Let’s Learn the Basic Colors
Fig. 4 Comparison of East African paleotemperature data with CMIP5/PMIP3 model output. Comparison of East African paleotemperature data with CMIP5/PMIP3.
Fig. 1 Study area and field site setting.
Stability and demographic responses of ant communities to warming
Fig. 2 Reconstructed global mean temperatures.
Fig. 1 Phase diagram and FS topologies.
Fig. 3 Forward model. Forward model. Summary of the resampled Monte Carlo simulations shown as histograms for epoch 1 (red), epoch 2 (green), and epoch.
Fig. 2 Images of complex structures formed via sequential folding.
Fig. 1 Time series and megadrought state changes.
Fig. 4 Identification of C
Fig. 4 Memristive characteristics in a 1T-TaS2 nano-thick crystal.
Fig. 3 ET dynamics on the control and treatment watersheds during the pretreatment and treatment periods. ET dynamics on the control and treatment watersheds.
Fig. 5 Wave speed analysis.
Fig. 3 Evolutions of freshwater transport and salinity.
Fig. 6 Global phase diagram.
Fig. 5 Most likely Neanderthal–modern human divergence time based on the analysis of phylogeny-1. Most likely Neanderthal–modern human divergence time.
by Cathryn A. Manduca, Ellen R. Iverson, Michael Luxenberg, R
Tony Lee, NASA JPL/CalTech
Fig. 3 Avoidable fraction of heat-related deaths if the current trajectory warming of 3°C is brought down to the 1.5° or 2°C Paris Agreement thresholds.
Fig. 2 Transient modeling results.
Fig. 1 Empirical probability density functions of the estimated climatic drivers. Empirical probability density functions of the estimated climatic drivers.
Relative impacts of mitigation, temperature, and precipitation on 21st-century megadrought risk in the American Southwest by Toby R. Ault, Justin S. Mankin,
Fig. 1 Influence of SSTA on the atmosphere and its relationship with U
Fig. 4 Relationships between light and economic parameters.
Fig. 5 Change in thermally suitable spawning habitat of Atlantic cod (left) and Polar cod (right) in the Seas of Norden under RCPs. Change in thermally.
Fig. 4 Theoretical analysis of the FeN4/GN structure and the catalytic reaction process by DFT calculations. Theoretical analysis of the FeN4/GN structure.
Fig. 1 Fractional coverage of the mapping method used in this study.
Fig. 3 Maximal energy intake.
Fig. 2 Comparison of the observed DRs and the estimates by the VR model and FL. Comparison of the observed DRs and the estimates by the VR model and FL.
Fig. 2 Number of years that would have been required for the observed vertebrate species extinctions in the last 114 years to occur under a background.
Fig. 1 Distribution of deformation and aqueous alteration in MIL
Fig. 10 Map of light pollution’s visual impact on the night sky.
SEM and TEM images and photoluminescence properties of composites
Fig. 2 Spatial distribution of five city groups.
Fig. 3 Global and basin-averaged sampling error compared with reconstructed temperature change. Global and basin-averaged sampling error compared with.
Fig. 4 Evolution of rate constants over varying interaction strengths.
Fig. 1 Uplift of the Isthmus of Panama and global sea levels over the last 20 My. Uplift of the Isthmus of Panama and global sea levels over the last 20.
Presentation transcript:

Fig. 1 AMOC stability in modern climate and AMOC response under global warming. AMOC stability in modern climate and AMOC response under global warming. (A) AMOC stability diagram where and are the AMOC stability indicators defined in Materials and Methods. The indicator values in modern climate are shown in solid circles for reanalysis data [Centro Euro-Mediterraneo sui Cambiamenti Climatici Global Ocean Physical Reanalysis System (C-GLORS; pink), Estimating the Circulation and Climate of the Ocean version 4 (ECCO-v4; brown), Ocean Reanalysis System 4 (ORAS4; green), and Simple Ocean Data Assimilation (SODA; yellow)], in gray triangles for the CMIP5 model simulations, and in blue and red diamonds for the CCSM3 CTL and ADJ runs. A positive or negative indicates that the AMOC resides in a stable or unstable regime. (B) , , and from reanalysis data, the CCSM3 CTL and ADJ runs with the same marker and color scheme as in (A), and the CMIP5 climate models in the form of the box-and-whisker plot. (C) Evolution of AMOC strength in the CTL (blue), CTLCO2 (light blue), ADJ (red), and ADJCO2 (orange), where the AMOC strength is defined as the maximum in the stream function below 500 m in the North Atlantic. A locally weighted scatterplot smoothing of 10-year intervals is applied to annual mean AMOC strength to remove interannual variability. Wei Liu et al. Sci Adv 2017;3:e1601666 Copyright © 2017, The Authors