Charles Galea (S3688570)
Last updated: 22 October, 2017
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Severe weather events and rising sea levels
Disease and population displacement
Unprecedent melting of glaciers and the polar ice caps.
Dramatic increase in atmospheric concentrations of carbon dioxide (CO\(_{2}\)) over the past century.
Atmospheric carbon dioxide traps heat leading to a Greenhouse Effect.
The Greenhouse Effect1 disrupts global weather patterns resulting in:
More frequent and severe weather events leading to natural disasters and population displacement.
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par(mfrow=c(2,2), mai=c(1, 1, 0.5, 1))
plot(CO2_levels ~ Date, data = CO2, xlab="Year", ylab = "CO2 conc (ppm)", col="blue", pch=16, cex=0.8, main="Carbon Dioxide Levels")
plot(GMSL ~ Year, data = sea_level, ylab = "sqrt(GMSL) (mm)", col="blue", pch=16, cex=0.8, main="Sea Levels")
plot(Temp_Change ~ Year, data = water, ylab = "Sea Surface Temp Anomaly (C)", col="blue", pch=16, cex=0.8, main="Sea Temp Anomalies")
plot(Temp_Change ~ Year, data = air, ylab = "Max Temp Anomaly (C)", col="blue", pch=16, cex=0.8, main="Max Ambient Temp Anomalies")par(mfrow=c(1,2))
plotNormalHistogram(water$Temp, col="antiquewhite2", main="Max Ambient Temperatures", linecol="blue2", xlab="")
plotNormalHistogram(air$Temp, col="antiquewhite2", main="Sea Surface Temperatures", linecol="blue2", xlab="") - Histograms of Maximum Ambient and Sea Surface Temperatures overlaid with a normal curve.
\(H_0:\) The data does not fit the linear regression model.
\(H_A:\) The data fits the linear regression model.
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Null Hypothesis - The intercept is equal to 0.
Alternate Hypothesis - The intercept is not equal to 0.
\[H_0: \alpha = 0 \]
\[H_A: \alpha \ne 0\]
Null Hypothesis - There was no relationship between x and y thus the slope is equal to 0.
Alternate Hypothesis - There was a relationship between x and y thus the slope is not equal to 0.
\[H_0: \beta = 0 \]
\[H_A: \beta \ne 0\]
Linear Regression Analysis
water_summary <- lm(Temp_Change ~ Year, data=water); water_summary %>% summary()##
## Call:
## lm(formula = Temp_Change ~ Year, data = water)
##
## Residuals:
## Min 1Q Median 3Q Max
## -0.46272 -0.11930 -0.01943 0.11359 0.43349
##
## Coefficients:
## Estimate Std. Error t value Pr(>|t|)
## (Intercept) -1.685e+01 9.216e-01 -18.29 <2e-16 ***
## Year 8.557e-03 4.706e-04 18.18 <2e-16 ***
## ---
## Signif. codes: 0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1
##
## Residual standard error: 0.1719 on 115 degrees of freedom
## Multiple R-squared: 0.7419, Adjusted R-squared: 0.7397
## F-statistic: 330.6 on 1 and 115 DF, p-value: < 2.2e-16
Confidence Interval
water_summary %>% confint()## 2.5 % 97.5 %
## (Intercept) -18.677271110 -15.026296754
## Year 0.007624816 0.009489183
Linear Regression Analysis
air_summary <- lm(Temp_Change ~ Year, data=air); air_summary %>% summary()##
## Call:
## lm(formula = Temp_Change ~ Year, data = air)
##
## Residuals:
## Min 1Q Median 3Q Max
## -0.8029 -0.2067 -0.0160 0.2398 0.7510
##
## Coefficients:
## Estimate Std. Error t value Pr(>|t|)
## (Intercept) -19.466859 2.102622 -9.258 2.83e-15 ***
## Year 0.009894 0.001071 9.238 3.14e-15 ***
## ---
## Signif. codes: 0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1
##
## Residual standard error: 0.3422 on 105 degrees of freedom
## Multiple R-squared: 0.4483, Adjusted R-squared: 0.4431
## F-statistic: 85.34 on 1 and 105 DF, p-value: 3.142e-15
Confidence Interval
air_summary %>% confint()## 2.5 % 97.5 %
## (Intercept) -23.635969044 -15.29774870
## Year 0.007770027 0.01201719
Correlation Coefficient
r <- cor(air$Temp_Change, air$Year, use = "complete.obs"); r## [1] 0.6695863
Confidence Intervals
library(psychometric); CIr(r, n = 107, level = .95)## [1] 0.5495962 0.7625095
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Correlation Coefficient
r <- cor(water$Temp_Change, water$Year, use = "complete.obs"); r## [1] 0.8613539
Confidence Intervals
CIr(r, n = 117, level = .95); detach("package:psychometric", unload=TRUE)## [1] 0.8058227 0.9018672
par(mfrow=c(1,2))
plot(Temp_Change ~ Year, data = water, ylab = "Sea Surface Temp Anomaly (C)", xlim=c(1880, 2017), ylim=c(-0.7, 1), col="blue", pch=16, cex=0.7, main="Sea Surface Temp")
abline(water_summary, col="red", lwd=2)
plot(Temp_Change ~ Year, data = air, ylab = "Max Temp Anomaly (C)", xlim=c(1880, 2017), ylim=c(-1.3, 1.4), col="blue", pch=16, cex=0.7, main="Max Ambient Temp")
abline(air_summary, col="red", lwd=2)par(mfrow=c(2,2)); plot(air_summary, col="blue", pch=16, lwd=2, cex=0.8)The residual vs fitted and square root or the standardized residuals plots indicate that this is a linear relationship and the data are homoscedastic.
The residuals vs leverage plot indicates no data points are outliers having a disproportionate influence on the fit of the regression model.
The qq-plot shows that the data fit a normal distribution.
par(mfrow=c(2,2)); plot(water_summary, col="blue", pch=16, lwd=2, cex=0.8)The residual vs fitted and square root or the standardized residuals plots indicate that this is a linear relationship and the data are homoscedastic.
The residuals vs leverage plot indicates no data points are outliers having a disproportionate influence on the fit of the regression model.
The qq-plot shows that the data fit a normal distribution.
- Atmospheric samples in ice cores show disproportionate increase in CO\(_{2}\) since the Industrial Revolution2,6.
Increased atmospheric CO\(_{2}\) levels have been proposed to lead to higher ambient temperatures.
We have shown a significant linear increase in Australian ambient maximum temperatures (~0.01\(^o\)C/year) and sea surface temperatures (~0.009\(^o\)C/year) over the past century.
Anticipated that increases in ambient temperatures will lead to further maleting of the poar ice caps contributing to rises in sea levels1.
- Studies have shown that sea levels have steadily risen of the past century.5
- By 2300 sea levels are predicted to increase to < 1m if CO\(_{2}\) levels are stabilized to < 500 ppm or could reach ~3m if levels rise above 700 ppm.
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Keeling, Charles D., Stephen C. Piper, Timothy P. Whorf, and Ralph F. Keeling Evolution of natural and anthropogenic fluxes of atmospheric CO\(_{2}\) from 1957 to 2003. Tellus B. 63 (2011): 1-22.
Australian Bureau of Meterology
Huang, B., V.F. Banzon, E. Freeman, J. Lawrimore, W. Liu, T.C. Peterson, T.M. Smith, P.W. Thorne, S.D. Woodruff, and H.-M. Zhang, 2015: Extended Reconstructed Sea Surface Temperature version 4 (ERSST.v4): Part I. Upgrades and intercomparisons. Journal of Climate 28:3, 911-930
Church, J. A. and N.J. White (2011), Sea-level rise from the late 19th to the early 21st Century. Surveys in Geophysics, 32, 585-602
Barnola J. M., Raynaud D., Korotkevich Y. S. and Lorius C. (1987) Vostok ice core provides 160,000-year record of atmospheric CO\(_{2}\). Nature, 329, 408-414