Canada vs Malaysia: Carbon Footprint of Bank Loans, Emissions intensities
Canada
87.51
in 2018
Malaysia
88.67
in 2018
Canada rank
18th
Malaysia rank
17th
Carbon Footprint of Bank Loans, Emissions intensities over time
- Canada
- Malaysia
How they compare
Malaysia currently reports 88.67 against 87.51 in Canada, a difference of 1.16.
The two have swapped places 2 times across 13 shared years of data; in 2006 it was Malaysia ahead.
Canada ranks 18th and Malaysia ranks 17th of 37 countries.
Malaysia has averaged higher in every one of the 2 decades both report.
Head to head by decade
| Decade | Canada | Malaysia | Difference | Ahead |
|---|---|---|---|---|
| 2000s | 81.19 | 123.69 | 42.5 | Malaysia |
| 2010s | 81.33 | 95.48 | 14.15 | Malaysia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher carbon footprint of bank loans, emissions intensities, Canada or Malaysia?
- Malaysia, at 88.67 against 87.51 in Canada as of 2018.
- What is the difference in carbon footprint of bank loans, emissions intensities between Canada and Malaysia?
- 1.16, with Malaysia ahead.
- How many years of comparable data are there for Canada and Malaysia?
- 13 years are reported by both, from 2006 to 2018.
- How do Canada and Malaysia rank globally for carbon footprint of bank loans, emissions intensities?
- Canada ranks 18th and Malaysia ranks 17th of 37 countries.
- Where does this data come from?
- International Monetary Fund, published as Carbon Footprint of Bank Loans, Emissions intensities (normalized). Statizoid refreshes it automatically from the source and publishes the full history for both places.
Individual pages
About this data
This dataset is designed to measure the carbon footprint of bank loans, which is a crucial component for understanding the environmental impact of financial portfolios. Bank loans provide finance to industries with varying degrees of carbon intensities. The footprint of bank loans contributes to the disclosure of the carbon intensity of the loans portfolio.