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Merge pull request #34 from explorable-viz/achintya-edits
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Replace <mark> with <a>, change CSS
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RaoOfPhysics authored Sep 9, 2024
2 parents 1e14fb6 + 553bc63 commit 1aeb090
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3 changes: 1 addition & 2 deletions css/styles.css
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Expand Up @@ -63,8 +63,7 @@ h4 {
}

a {
text-decoration: none;
color: inherit;
border-bottom: lightblue 0.1em solid;
transition-timing-function: ease-out
}

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6 changes: 3 additions & 3 deletions index.html
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Expand Up @@ -36,13 +36,13 @@ <h2 class="title">
Scenario: Without climate change mitigation but with stringent air pollution control (SSP5-8.5)
</h2>
<p>
At the same time, the <mark>SSP scenarios without climate change mitigation</mark> project <mark>faster growth in methane emissions in Africa, the Middle East</mark> and Latin America (Figure 6.19) driven by <mark>developments in agriculture, the oil and gas sectors, and, especially in Africa, waste management</mark>.
At the same time, the <a>SSP scenarios without climate change mitigation</a> project <a>faster growth in methane emissions in Africa, the Middle East</a> and Latin America (Figure 6.19) driven by <a>developments in agriculture, the oil and gas sectors, and […] waste management</a>.
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<p>
After 2050, surface ozone concentrations decrease in SSP5-8.5, reaching levels below their 2005–2014 mean levels in most regions, but level off or continue to increase under SSP3-7.0. The increase in surface ozone in the <mark>SSP5-8.5 scenario</mark> occurs despite an emissions decrease of several ozone precursors <mark>because the methane emissions increase until about 2080</mark> in the absence of climate change mitigation.
After 2050, surface ozone concentrations decrease in SSP5-8.5, reaching levels below their 2005–2014 mean levels in most regions, but level off or continue to increase under SSP3-7.0. The increase in surface ozone in the <a>SSP5-8.5 scenario</a> occurs despite an emissions decrease of several ozone precursors <a>because the methane emissions increase until about 2080</a> in the absence of climate change mitigation.
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<p>
In <mark>SSP5-8.5, methane emissions increase</mark> in North America, Europe and <mark>Africa</mark>, while there is a decrease in the Asian regions. For North America and Europe, the methane increase combined with a reduction in aerosol leads to highest net contribution to GSAT in this scenario (0.06°C and 0.04°C in 2100, respectively). The <mark>high growth in methane makes Africa the region with the largest contribution to future warming</mark> by SLCFs (0.18°C in 2100 versus 2020) in this scenario.
In <a>SSP5-8.5, methane emissions increase</a> in North America, Europe and <a>Africa</a>, while there is a decrease in the Asian regions. For North America and Europe, the methane increase combined with a reduction in aerosol leads to highest net contribution to GSAT in this scenario (0.06°C and 0.04°C in 2100, respectively). The <a>high growth in methane makes Africa the region with the largest contribution to future warming</a> by SLCFs (0.18°C in 2100 versus 2020) in this scenario.
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