There have been many studies documenting that the average global temperature has been increasing over the last century. The consequences of a continued rise in global temperature will be dire. Rising sea levels and an increased frequency of extreme weather events will affect billions of people.
In this analysis, I’ll attempt to study the relationship between average global temperature and several other factors.
The file climate_change.csv contains climate data from May 1983 to December 2008. The available variables include:
- Year: the observation year.
- Month: the observation month.
- Temp: the difference in degrees Celsius between the average global temperature in that period and a reference value. This data comes from the Climatic Research Unit at the University of East Anglia.
- CO2, N2O, CH4, CFC.11, CFC.12: atmospheric concentrations of carbon dioxide (CO2), nitrous oxide (N2O), methane (CH4), trichlorofluoromethane (CCl3F; commonly referred to as CFC-11) and dichlorodifluoromethane (CCl2F2; commonly referred to as CFC-12), respectively. This data comes from the ESRL/NOAA Global Monitoring Division.
- CO2, N2O and CH4 are expressed in ppmv (parts per million by volume – i.e., 397 ppmv of CO2 means that CO2 constitutes 397 millionths of the total volume of the atmosphere)
- CFC.11 and CFC.12 are expressed in ppbv (parts per billion by volume).
- Aerosols: the mean stratospheric aerosol optical depth at 550 nm. This variable is linked to volcanoes, as volcanic eruptions result in new particles being added to the atmosphere, which affect how much of the sun’s energy is reflected back into space. This data is from the Godard Institute for Space Studies at NASA.
- TSI: the total solar irradiance (TSI) in W/m2 (the rate at which the sun’s energy is deposited per unit area). Due to sunspots and other solar phenomena, the amount of energy that is given off by the sun varies substantially with time. This data is from the SOLARIS-HEPPA project website.
- MEI: multivariate El Nino Southern Oscillation index (MEI), a measure of the strength of the El Nino/La Nina-Southern Oscillation (a weather effect in the Pacific Ocean that affects global temperatures). This data comes from the ESRL/NOAA Physical Sciences Division.
We are interested in how changes in these variables affect future temperatures, as well as how well these variables explain temperature changes so far. To do this, first read the dataset climate_change.csv.
climate <- read.csv("climate_change.csv")
str(climate)
'data.frame': 308 obs. of 11 variables:
$ Year : int 1983 1983 1983 1983 1983 1983 1983 1983 1984 1984 ...
$ Month : int 5 6 7 8 9 10 11 12 1 2 ...
$ MEI : num 2.556 2.167 1.741 1.13 0.428 ...
$ CO2 : num 346 346 344 342 340 ...
$ CH4 : num 1639 1634 1633 1631 1648 ...
$ N2O : num 304 304 304 304 304 ...
$ CFC.11 : num 191 192 193 194 194 ...
$ CFC.12 : num 350 352 354 356 357 ...
$ TSI : num 1366 1366 1366 1366 1366 ...
$ Aerosols: num 0.0863 0.0794 0.0731 0.0673 0.0619 0.0569 0.0524 0.0486 0.0451 0.0416 ...
$ Temp : num 0.109 0.118 0.137 0.176 0.149 0.093 0.232 0.078 0.089 0.013 ...
summary(climate)
Year Month MEI CO2
Min. :1983 Min. : 1.000 Min. :-1.6350 Min. :340.2
1st Qu.:1989 1st Qu.: 4.000 1st Qu.:-0.3987 1st Qu.:353.0
Median :1996 Median : 7.000 Median : 0.2375 Median :361.7
Mean :1996 Mean : 6.552 Mean : 0.2756 Mean :363.2
3rd Qu.:2002 3rd Qu.:10.000 3rd Qu.: 0.8305 3rd Qu.:373.5
Max. :2008 Max. :12.000 Max. : 3.0010 Max. :388.5
CH4 N2O CFC.11 CFC.12
Min. :1630 Min. :303.7 Min. :191.3 Min. :350.1
1st Qu.:1722 1st Qu.:308.1 1st Qu.:246.3 1st Qu.:472.4
Median :1764 Median :311.5 Median :258.3 Median :528.4
Mean :1750 Mean :312.4 Mean :252.0 Mean :497.5
3rd Qu.:1787 3rd Qu.:317.0 3rd Qu.:267.0 3rd Qu.:540.5
Max. :1814 Max. :322.2 Max. :271.5 Max. :543.8
TSI Aerosols Temp
Min. :1365 Min. :0.00160 Min. :-0.2820
1st Qu.:1366 1st Qu.:0.00280 1st Qu.: 0.1217
Median :1366 Median :0.00575 Median : 0.2480
Mean :1366 Mean :0.01666 Mean : 0.2568
3rd Qu.:1366 3rd Qu.:0.01260 3rd Qu.: 0.4073
Max. :1367 Max. :0.14940 Max. : 0.7390
ML Workflow
Then, split the data into a training set, consisting of all the observations up to and including 2006, and a testing set consisting of the remaining years (hint: use subset). A training set refers to the data that will be used to build the model (this is the data we give to the lm() function), and a testing set refers to the data we will use to test our predictive ability.
climate_train <- subset(climate, Year <= 2006)
climate_test <- subset(climate, Year > 2006)
str(climate_train)
'data.frame': 284 obs. of 11 variables:
$ Year : int 1983 1983 1983 1983 1983 1983 1983 1983 1984 1984 ...
$ Month : int 5 6 7 8 9 10 11 12 1 2 ...
$ MEI : num 2.556 2.167 1.741 1.13 0.428 ...
$ CO2 : num 346 346 344 342 340 ...
$ CH4 : num 1639 1634 1633 1631 1648 ...
$ N2O : num 304 304 304 304 304 ...
$ CFC.11 : num 191 192 193 194 194 ...
$ CFC.12 : num 350 352 354 356 357 ...
$ TSI : num 1366 1366 1366 1366 1366 ...
$ Aerosols: num 0.0863 0.0794 0.0731 0.0673 0.0619 0.0569 0.0524 0.0486 0.0451 0.0416 ...
$ Temp : num 0.109 0.118 0.137 0.176 0.149 0.093 0.232 0.078 0.089 0.013 ...
summary(climate_train)
Year Month MEI CO2
Min. :1983 Min. : 1.000 Min. :-1.5860 Min. :340.2
1st Qu.:1989 1st Qu.: 4.000 1st Qu.:-0.3230 1st Qu.:352.3
Median :1995 Median : 7.000 Median : 0.3085 Median :359.9
Mean :1995 Mean : 6.556 Mean : 0.3419 Mean :361.4
3rd Qu.:2001 3rd Qu.:10.000 3rd Qu.: 0.8980 3rd Qu.:370.6
Max. :2006 Max. :12.000 Max. : 3.0010 Max. :385.0
CH4 N2O CFC.11 CFC.12
Min. :1630 Min. :303.7 Min. :191.3 Min. :350.1
1st Qu.:1716 1st Qu.:307.7 1st Qu.:249.6 1st Qu.:462.5
Median :1759 Median :310.8 Median :260.4 Median :522.1
Mean :1746 Mean :311.7 Mean :252.5 Mean :494.2
3rd Qu.:1782 3rd Qu.:316.1 3rd Qu.:267.4 3rd Qu.:541.0
Max. :1808 Max. :320.5 Max. :271.5 Max. :543.8
TSI Aerosols Temp
Min. :1365 Min. :0.00160 Min. :-0.2820
1st Qu.:1366 1st Qu.:0.00270 1st Qu.: 0.1180
Median :1366 Median :0.00620 Median : 0.2325
Mean :1366 Mean :0.01772 Mean : 0.2478
3rd Qu.:1366 3rd Qu.:0.01400 3rd Qu.: 0.4065
Max. :1367 Max. :0.14940 Max. : 0.7390
str(climate_test)
'data.frame': 24 obs. of 11 variables:
$ Year : int 2007 2007 2007 2007 2007 2007 2007 2007 2007 2007 ...
$ Month : int 1 2 3 4 5 6 7 8 9 10 ...
$ MEI : num 0.974 0.51 0.074 -0.049 0.183 ...
$ CO2 : num 383 384 385 386 387 ...
$ CH4 : num 1800 1803 1803 1802 1796 ...
$ N2O : num 321 321 321 321 320 ...
$ CFC.11 : num 248 248 248 248 247 ...
$ CFC.12 : num 539 539 539 539 538 ...
$ TSI : num 1366 1366 1366 1366 1366 ...
$ Aerosols: num 0.0054 0.0051 0.0045 0.0045 0.0041 0.004 0.004 0.0041 0.0042 0.0041 ...
$ Temp : num 0.601 0.498 0.435 0.466 0.372 0.382 0.394 0.358 0.402 0.362 ...
summary(climate_test)
Year Month MEI CO2
Min. :2007 Min. : 1.00 Min. :-1.6350 Min. :380.9
1st Qu.:2007 1st Qu.: 3.75 1st Qu.:-1.0437 1st Qu.:383.1
Median :2008 Median : 6.50 Median :-0.5305 Median :384.5
Mean :2008 Mean : 6.50 Mean :-0.5098 Mean :384.7
3rd Qu.:2008 3rd Qu.: 9.25 3rd Qu.:-0.0360 3rd Qu.:386.1
Max. :2008 Max. :12.00 Max. : 0.9740 Max. :388.5
CH4 N2O CFC.11 CFC.12
Min. :1772 Min. :320.3 Min. :244.1 Min. :534.9
1st Qu.:1792 1st Qu.:320.6 1st Qu.:244.6 1st Qu.:535.1
Median :1798 Median :321.3 Median :246.2 Median :537.0
Mean :1797 Mean :321.1 Mean :245.9 Mean :536.7
3rd Qu.:1804 3rd Qu.:321.4 3rd Qu.:246.6 3rd Qu.:537.4
Max. :1814 Max. :322.2 Max. :248.4 Max. :539.2
TSI Aerosols Temp
Min. :1366 Min. :0.003100 Min. :0.074
1st Qu.:1366 1st Qu.:0.003600 1st Qu.:0.307
Median :1366 Median :0.004100 Median :0.380
Mean :1366 Mean :0.004071 Mean :0.363
3rd Qu.:1366 3rd Qu.:0.004500 3rd Qu.:0.414
Max. :1366 Max. :0.005400 Max. :0.601
Next, build a linear regression model to predict the dependent variable Temp, using MEI, CO2, CH4, N2O, CFC.11, CFC.12, TSI, and Aerosols as independent variables (Year and Month should NOT be used in the model). Use the training set to build the model.
fit.climate <-
lm(Temp ~ MEI + CO2 + CH4 + N2O + CFC.11 + CFC.12 + TSI + Aerosols,
data = climate_train)
summary(fit.climate)
Call:
lm(formula = Temp ~ MEI + CO2 + CH4 + N2O + CFC.11 + CFC.12 +
TSI + Aerosols, data = climate_train)
Residuals:
Min 1Q Median 3Q Max
-0.25888 -0.05913 -0.00082 0.05649 0.32433
Coefficients:
Estimate Std. Error t value Pr(>|t|)
(Intercept) -1.246e+02 1.989e+01 -6.265 1.43e-09 ***
MEI 6.421e-02 6.470e-03 9.923 < 2e-16 ***
CO2 6.457e-03 2.285e-03 2.826 0.00505 **
CH4 1.240e-04 5.158e-04 0.240 0.81015
N2O -1.653e-02 8.565e-03 -1.930 0.05467 .
CFC.11 -6.631e-03 1.626e-03 -4.078 5.96e-05 ***
CFC.12 3.808e-03 1.014e-03 3.757 0.00021 ***
TSI 9.314e-02 1.475e-02 6.313 1.10e-09 ***
Aerosols -1.538e+00 2.133e-01 -7.210 5.41e-12 ***
---
Signif. codes: 0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1
Residual standard error: 0.09171 on 275 degrees of freedom
Multiple R-squared: 0.7509, Adjusted R-squared: 0.7436
F-statistic: 103.6 on 8 and 275 DF, p-value: < 2.2e-16
The model R2 (the “Multiple R-squared” value) is 0.7509
Creating Our First Model
Which variables are significant in the model? We will consider a variable signficant only if the p-value is below 0.05. #### MEI, CO2, CFC.11, CFC.12, TSI, Aerosols
Understanding the Model
Current scientific opinion is that nitrous oxide and CFC-11 are greenhouse gases: gases that are able to trap heat from the sun and contribute to the heating of the Earth. However, the regression coefficients of both the N2O and CFC-11 variables are negative, indicating that increasing atmospheric concentrations of either of these two compounds is associated with lower global temperatures.
Which of the following is the simplest correct explanation for this contradiction? #### All of the gas concentration variables reflect human development - N2O and CFC.11 are correlated with other variables in the dataset.
Compute the correlations between all the variables in the training set.
cor(climate_train)
Year Month MEI CO2 CH4
Year 1.00000000 -0.0279419602 -0.0369876842 0.98274939 0.91565945
Month -0.02794196 1.0000000000 0.0008846905 -0.10673246 0.01856866
MEI -0.03698768 0.0008846905 1.0000000000 -0.04114717 -0.03341930
CO2 0.98274939 -0.1067324607 -0.0411471651 1.00000000 0.87727963
CH4 0.91565945 0.0185686624 -0.0334193014 0.87727963 1.00000000
N2O 0.99384523 0.0136315303 -0.0508197755 0.97671982 0.89983864
CFC.11 0.56910643 -0.0131112236 0.0690004387 0.51405975 0.77990402
CFC.12 0.89701166 0.0006751102 0.0082855443 0.85268963 0.96361625
TSI 0.17030201 -0.0346061935 -0.1544919227 0.17742893 0.24552844
Aerosols -0.34524670 0.0148895406 0.3402377871 -0.35615480 -0.26780919
Temp 0.78679714 -0.0998567411 0.1724707512 0.78852921 0.70325502
N2O CFC.11 CFC.12 TSI Aerosols
Year 0.99384523 0.56910643 0.8970116635 0.17030201 -0.34524670
Month 0.01363153 -0.01311122 0.0006751102 -0.03460619 0.01488954
MEI -0.05081978 0.06900044 0.0082855443 -0.15449192 0.34023779
CO2 0.97671982 0.51405975 0.8526896272 0.17742893 -0.35615480
CH4 0.89983864 0.77990402 0.9636162478 0.24552844 -0.26780919
N2O 1.00000000 0.52247732 0.8679307757 0.19975668 -0.33705457
CFC.11 0.52247732 1.00000000 0.8689851828 0.27204596 -0.04392120
CFC.12 0.86793078 0.86898518 1.0000000000 0.25530281 -0.22513124
TSI 0.19975668 0.27204596 0.2553028138 1.00000000 0.05211651
Aerosols -0.33705457 -0.04392120 -0.2251312440 0.05211651 1.00000000
Temp 0.77863893 0.40771029 0.6875575483 0.24338269 -0.38491375
Temp
Year 0.78679714
Month -0.09985674
MEI 0.17247075
CO2 0.78852921
CH4 0.70325502
N2O 0.77863893
CFC.11 0.40771029
CFC.12 0.68755755
TSI 0.24338269
Aerosols -0.38491375
Temp 1.00000000
The following independent variables is N2O, highly correlated with (absolute correlation greater than 0.7)? #### CO2, CH4, CFC.12
The following independent variables is CFC.11, highly correlated with? #### CH4, CFC.12
Simplifying the Model
Given that the correlations are so high, let us focus on the N2O variable and build a model with only MEI, TSI, Aerosols and N2O as independent variables. Note, using the training set to build the model.
fit.climate.2 <-
lm(Temp ~ MEI + N2O + TSI + Aerosols,
data = climate_train)
summary(fit.climate.2)
Call:
lm(formula = Temp ~ MEI + N2O + TSI + Aerosols, data = climate_train)
Residuals:
Min 1Q Median 3Q Max
-0.27916 -0.05975 -0.00595 0.05672 0.34195
Coefficients:
Estimate Std. Error t value Pr(>|t|)
(Intercept) -1.162e+02 2.022e+01 -5.747 2.37e-08 ***
MEI 6.419e-02 6.652e-03 9.649 < 2e-16 ***
N2O 2.532e-02 1.311e-03 19.307 < 2e-16 ***
TSI 7.949e-02 1.487e-02 5.344 1.89e-07 ***
Aerosols -1.702e+00 2.180e-01 -7.806 1.19e-13 ***
---
Signif. codes: 0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1
Residual standard error: 0.09547 on 279 degrees of freedom
Multiple R-squared: 0.7261, Adjusted R-squared: 0.7222
F-statistic: 184.9 on 4 and 279 DF, p-value: < 2.2e-16
The coefficient of N2O in this reduced model is 2.532e-02
(How does this compare to the coefficient in the previous model with all of the variables?) The model R2 is 0.7261
Automatically Building the Model
We have many variables in this analysis, and as we have seen above, dropping some from the model does not decrease model quality. R provides a function, step, that will automate the procedure of trying different combinations of variables to find a good compromise of model simplicity and R2.
This trade-off is formalized by the Akaike information criterion (AIC) - it can be informally thought of as the quality of the model with a penalty for the number of variables in the model.
The step function has one argument - the name of the initial model. It returns a simplified model. Using the step function in R to derive a new model, with the full model as the initial model (HINT: If your initial full model was called “climateLM”, you could create a new model with the step function by typing step(climateLM). Be sure to save your new model to a variable name so that you can look at the summary. For more information about the step function, type? step in your R console.)
fit.climate.step <- step(fit.climate)
Start: AIC=-1348.16
Temp ~ MEI + CO2 + CH4 + N2O + CFC.11 + CFC.12 + TSI + Aerosols
Df Sum of Sq RSS AIC
- CH4 1 0.00049 2.3135 -1350.1
<none> 2.3130 -1348.2
- N2O 1 0.03132 2.3443 -1346.3
- CO2 1 0.06719 2.3802 -1342.0
- CFC.12 1 0.11874 2.4318 -1335.9
- CFC.11 1 0.13986 2.4529 -1333.5
- TSI 1 0.33516 2.6482 -1311.7
- Aerosols 1 0.43727 2.7503 -1301.0
- MEI 1 0.82823 3.1412 -1263.2
Step: AIC=-1350.1
Temp ~ MEI + CO2 + N2O + CFC.11 + CFC.12 + TSI + Aerosols
Df Sum of Sq RSS AIC
<none> 2.3135 -1350.1
- N2O 1 0.03133 2.3448 -1348.3
- CO2 1 0.06672 2.3802 -1344.0
- CFC.12 1 0.13023 2.4437 -1336.5
- CFC.11 1 0.13938 2.4529 -1335.5
- TSI 1 0.33500 2.6485 -1313.7
- Aerosols 1 0.43987 2.7534 -1302.7
- MEI 1 0.83118 3.1447 -1264.9
summary(fit.climate.step)
Call:
lm(formula = Temp ~ MEI + CO2 + N2O + CFC.11 + CFC.12 + TSI +
Aerosols, data = climate_train)
Residuals:
Min 1Q Median 3Q Max
-0.25770 -0.05994 -0.00104 0.05588 0.32203
Coefficients:
Estimate Std. Error t value Pr(>|t|)
(Intercept) -1.245e+02 1.985e+01 -6.273 1.37e-09 ***
MEI 6.407e-02 6.434e-03 9.958 < 2e-16 ***
CO2 6.402e-03 2.269e-03 2.821 0.005129 **
N2O -1.602e-02 8.287e-03 -1.933 0.054234 .
CFC.11 -6.609e-03 1.621e-03 -4.078 5.95e-05 ***
CFC.12 3.868e-03 9.812e-04 3.942 0.000103 ***
TSI 9.312e-02 1.473e-02 6.322 1.04e-09 ***
Aerosols -1.540e+00 2.126e-01 -7.244 4.36e-12 ***
---
Signif. codes: 0 '***' 0.001 '**' 0.01 '*' 0.05 '.' 0.1 ' ' 1
Residual standard error: 0.09155 on 276 degrees of freedom
Multiple R-squared: 0.7508, Adjusted R-squared: 0.7445
F-statistic: 118.8 on 7 and 276 DF, p-value: < 2.2e-16
R2 value of the model produced by the step function is 0.7508
Which of the following variable(s) were eliminated from the full model by the step function? #### It is interesting to note that the step function does not address the collinearity of the variables, except that adding highly correlated variables will not improve the R2 significantly. The consequence of this is that the step function will not necessarily produce a very interpretable model - just a model that has balanced quality and simplicity for a particular weighting of quality and simplicity (AIC).
Testing on Unseen Data
We have developed an understanding of how well we can fit a linear regression to the training data, but does the model quality hold when applied to unseen data?
Using the model produced from the step function, calculate temperature predictions for the testing dataset, using the predict function.
TempPredictions <- predict(fit.climate.step, newdata = climate_test)
climate.SSE = sum((TempPredictions - climate_test$Temp)^2)
climate.SST = sum((climate_test$Temp - mean(climate_train$Temp))^2)
1 - climate.SSE/climate.SST
[1] 0.6286051
Testing set R2 is 0.6286