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refactor

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baol 2023-11-13 10:52:17 +08:00
parent 4ad99f7037
commit 80a9d15884
1 changed files with 27 additions and 27 deletions
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54
src/components/home/Layout/NavBar.jsx
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@ -78,7 +78,7 @@ const itemsFour = [
key: "1",
label: (
<a target="_blank" rel="noopener noreferrer" href="/show/map/1">
两极协同—拉布拉多海海温偏暖控制夏季高原年代际增温
拉布拉多海海温偏暖控制夏季高原年代际增温
</a>
),
},
@ -86,7 +86,7 @@ const itemsFour = [
key: "2",
label: (
<a target="_blank" rel="noopener noreferrer" href="/show/map/2">
两极协同—南极涛动有效调节青藏高原降水和加热
南极涛动有效调节青藏高原降水和加热
</a>
),
},
@ -94,34 +94,34 @@ const itemsFour = [
key: "3",
label: (
<a target="_blank" rel="noopener noreferrer" href="/show/map/3">
两极协同—连接南极和北极的热带大西洋经向模的媒介作用
</a>
),
},
{
key: "4",
label: (
<a target="_blank" rel="noopener noreferrer" href="/show/map/4">
三极联动影响青藏高原上层温度
</a>
),
},
{
key: "5",
label: (
<a target="_blank" rel="noopener noreferrer" href="/show/map/5">
三极联动影响东亚夏季风
</a>
),
},
{
key: "6",
label: (
<a target="_blank" rel="noopener noreferrer" href="/show/map/6">
三极冰盖/冰川表面冰雪冻融对比关联与科学认知
连接南极和北极的热带大西洋经向模的媒介作用
</a>
),
},
// {
// key: "4",
// label: (
// <a target="_blank" rel="noopener noreferrer" href="/show/map/4">
// 三极联动影响青藏高原上层温度
// </a>
// ),
// },
// {
// key: "5",
// label: (
// <a target="_blank" rel="noopener noreferrer" href="/show/map/5">
// 三极联动影响东亚夏季风
// </a>
// ),
// },
// {
// key: "6",
// label: (
// <a target="_blank" rel="noopener noreferrer" href="/show/map/6">
// 三极冰盖/冰川表面冰雪冻融对比关联与科学认知
// </a>
// ),
// },
];
function NavBar() {