10 Abubuwan Ban Sha'awa About Paleoclimatology and climate change

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• FaleoCiminomology shine binciken canjin yanayi a baya.
• Dangane da bayanan Faleocliology, yawan zafin jiki na duniya a baya ya kasance mai sanyi fiye da yanzu.
• A cikin shekaru 800 da suka gabata, abun ciki na carbon dioxide a cikin yanayin duniya bai taba kai 300 ppm (yanzu a yanzu miliyan) ya wuce 400 ppm.
• A cewar binciken Paleclisolat, a halin yanzu canjin yanayi a halin yanzu idan aka kwatanta da canjin yanayi a baya.
• Masanin almara suna amfani da nau'ikan shaidu daban-daban don nazarin canjin yanayi a baya, kamar kankara, duwatsun, da burbushin, da burbushin.
• Canjin yanayi yanzu yana da tasiri ga yanayin muhalli, kamar karuwar zazzabi, karuwa a matakin teku, da kuma yawan bala'i da ke kara yawan gaske.
• A cewar bincike na Faleochatal, canjin yanayi na iya haifar da manyan canje-canje a cikin muhalli kuma yana shafar juyin halitta na rayuwar rayuwa ta gaba.
• Wasu nau'ikan dabbobi da tsire-tsire sun samo asali don tsira cikin matsanancin yanayin yanayi a baya.
• Canjin yanayi na yanzu yana iya haifar da canja wurin dabba da shuka nau'in da aka sanyaya waƙar ko yanki mai zafi.
• Masana ilimi suna ci gaba da yin nazarin canjin yanayi a baya don fahimtar mafi kyawun canjin yanayi na yanzu kuma yin annabci abin da zai faru nan gaba.