Presentation is loading. Please wait.

Presentation is loading. Please wait.

Hawkings et al. The effect of warming climate on nutrient and solute export from the Greenland Ice Sheet Figure S-4 Comparison of regression plots for.

Published byJustin Rodger Parks Modified over 6 years ago

Similar presentations

Presentation on theme: "Hawkings et al. The effect of warming climate on nutrient and solute export from the Greenland Ice Sheet Figure S-4 Comparison of regression plots for."— Presentation transcript:

1 Hawkings et al. The effect of warming climate on nutrient and solute export from the Greenland Ice Sheet Figure S-4 Comparison of regression plots for the major ions for 2009, 2010 and 2012, where data are available. The differences in the regression equations used to determine major ion concentrations are very small. Figure S-4 Comparison of regression plots for the major ions for 2009, 2010 and 2012, where data are available. The differences in the regression equations used to determine major ion concentrations are very small. Hawkings et al. (2015) Geochem. Persp. Let. 1, | doi: /geochemlet.1510 © 2015 European Association of Geochemistry

Download ppt "Hawkings et al. The effect of warming climate on nutrient and solute export from the Greenland Ice Sheet Figure S-4 Comparison of regression plots for."

Similar presentations

Figure S-2 Zircon U-Pb age distribution for detrital zircons from North & Central America, Australia, Europe, South America, Africa, Asia and India using.

Figure S-2 Zircon U-Pb age distribution for detrital zircons from North & Central America, Australia, Europe, South America, Africa, Asia and India using.
Oceanography & Climate Synthesis Question: If all of the oceans currents changed direction, would they then heat the equator and cool the poles?

Oceanography & Climate Synthesis Question: If all of the oceans currents changed direction, would they then heat the equator and cool the poles?
P247. Figure 9-1 p248 Figure 9-2 p251 p251 Figure 9-3 p253.

P247. Figure 9-1 p248 Figure 9-2 p251 p251 Figure 9-3 p253.
Graph an equation in standard form

Graph an equation in standard form
Linear Equations, Inequalities, and Absolute Value

Linear Equations, Inequalities, and Absolute Value
Solving Quadratic Equations by Factoring. Solution by factoring Example 1 Find the roots of each quadratic by factoring. factoring a) x² − 3x + 2 b) x².

Solving Quadratic Equations by Factoring. Solution by factoring Example 1 Find the roots of each quadratic by factoring. factoring a) x² − 3x + 2 b) x².
Warm up: solve for x x – (-2) = -13. Inverse Operations LEQ: What are inverse operations and how do we use them to solve one step equations?

Warm up: solve for x x – (-2) = -13. Inverse Operations LEQ: What are inverse operations and how do we use them to solve one step equations?
Analytical Solutions of Poisson's Equation for Realistic Geometrical Shapes of Membrane Ion Channels Serdar Kuyucak, Matthew Hoyles, Shin-Ho Chung Biophysical.

Analytical Solutions of Poisson's Equation for Realistic Geometrical Shapes of Membrane Ion Channels Serdar Kuyucak, Matthew Hoyles, Shin-Ho Chung Biophysical.
Warm Up  1.) Write 15x 2 + 6x = 14x 2 -12 in standard form. (ax 2 + bx + c = 0)  2.) Evaluate b 2 – 4ac when a = 3, b = -6, and c = 5.

Warm Up  1.) Write 15x 2 + 6x = 14x in standard form. (ax 2 + bx + c = 0)  2.) Evaluate b 2 – 4ac when a = 3, b = -6, and c = 5.
2( ) 8x + 14y = 4 -12x – 14y = -20 -4x = -16 -4 x = 4 8x + 14y = 4 8(4) + 14y =4 32 + 14y = 4 -32 14y = -28 ___ ___ 14 14 y = -2 The solution is (4, -2)

2( ) 8x + 14y = 4 -12x – 14y = x = x = 4 8x + 14y = 4 8(4) + 14y = y = y = -28 ___ ___ y = -2 The solution is (4, -2)
Creech et al. Late accretion history of the terrestrial planets inferred from platinum stable isotopes Figure 3 Model of the effect of addition of chondritic.

Creech et al. Late accretion history of the terrestrial planets inferred from platinum stable isotopes Figure 3 Model of the effect of addition of chondritic.
The solubility of heat-producing elements in Earth’s core

The solubility of heat-producing elements in Earth’s core
Distribution of Zn isotopes during Alzheimer’s disease

Distribution of Zn isotopes during Alzheimer’s disease
Direct sensing of total alkalinity profile in a stratified lake

Direct sensing of total alkalinity profile in a stratified lake
Van Hinsberg et al. Determining subduction-zone fluid composition using a tourmaline mineral probe Figure 1 Reading the Tauern tourmaline record. (a)

Van Hinsberg et al. Determining subduction-zone fluid composition using a tourmaline mineral probe Figure 1 Reading the Tauern tourmaline record. (a)
Van Hinsberg et al. Determining subduction-zone fluid composition using a tourmaline mineral probe Figure S-3 Reconstructed Ba/Th vs. La/Sm ratios for.

Van Hinsberg et al. Determining subduction-zone fluid composition using a tourmaline mineral probe Figure S-3 Reconstructed Ba/Th vs. La/Sm ratios for.
Dahl et al. Reorganisation of Earth’s biogeochemical cycles briefly oxygenated the oceans 520 Myr ago Figure 3 Conceptual model for the episodic expansion.

Dahl et al. Reorganisation of Earth’s biogeochemical cycles briefly oxygenated the oceans 520 Myr ago Figure 3 Conceptual model for the episodic expansion.
Schiller et al. Tracking the formation of magma oceans in the Solar System using stable magnesium isotopes Figure 1 The minimum degree of partial melting.

Schiller et al. Tracking the formation of magma oceans in the Solar System using stable magnesium isotopes Figure 1 The minimum degree of partial melting.
Solving and Graphing Inequalities

Solving and Graphing Inequalities
Morin et al. Mononuclear U(IV) complexes and ningyoite as major uranium species in lake sediments Figure 4 (a) Concentration of U(IV) extracted by O2-free.

Morin et al. Mononuclear U(IV) complexes and ningyoite as major uranium species in lake sediments Figure 4 (a) Concentration of U(IV) extracted by O2-free.

Similar presentations

Ads by Google