Journal of Infrared and Millimeter Waves, Volume. 43, Issue 3, 397(2024)
Arctic sea surface CO2 partial pressure based on LiDAR
Fig. 1. Flowchart of the FNN-LID day/night sea surface pCO2 retrieved method.
Fig. 2. Comparison between CALIPSO-Chla and BGC-argo of global Chla (μg L-1).
Fig. 3. Sea Water Chla concentrate (μg L-1) from (a) MODIS and (b) CALIPSO on December 2011. White indicates invalid data areas,while light gray shading represents sea ice
Fig. 4. Seasonal distribution of climate-averaged sea surface Chla concentrate for Arctic Ocean (μg L-1): (a) Spring (March-May) ; (b) Summer (June-August) ;(c) Autumn (September-November),and (d) Winter (December-February)
Fig. 5. Comparison between CALIPSO-pCO2 and with observed data in the validation set (µatm).
Fig. 6. Seasonal distribution of climate-averaged sea surface pCO2 for Arctic Ocean (μatm): (a) Spring (March-May) ; (b) Summer (June-August) ;(c) Autumn (September-November) ;and (d) Winter (December-February)
Fig. 7. Seasonal variation of atmospheric and sea surface pCO2 in the Arctic Ocean.
Fig. 8. Long-term variation of pCO2 in different Subregions of the Arctic Ocean.
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Si-Qi ZHANG, Peng CHEN, Zhen-Hua ZHANG, De-Lu PAN. Arctic sea surface CO2 partial pressure based on LiDAR[J]. Journal of Infrared and Millimeter Waves, 2024, 43(3): 397
Category: Research Articles
Received: Oct. 7, 2023
Accepted: --
Published Online: Apr. 29, 2024
The Author Email: Peng CHEN (chenp@sio.org.cn)