MIS13时期黄土高原东西部地区夏季风不对称演化
根据黄土高原中东部地区黄土沉积物的地质记录，前人研究推断MIS13时期北半球气候为高温高湿环境，然而，这似乎与黄土高原西部黄土沉积物的地质记录存在差别。本研究通过综合前人的研究结果，对比黄土高原东西部地区MIS13时期的古气候及古土壤风化强度在空间上的梯度分布，发现两地的古气候演化存在不对称性。对比MIS13时期低纬度的亚非季风区和北半球中高纬度地区气候状况得出：高降水量环境仅存在于亚非季风区大部分地区，但当时是否呈现高温环境值得商榷；北半球中高纬地区则显著不同，呈现相对较干冷的间冰期气候。由此推断，MIS13时期黄土高原东西部地区之间气候演化的不对称现象可能是季风缺少动力因素，对黄土高原西部...
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| Published in | Hăiyang dĭzhĭ yu dĭsĭjĭ dĭzhĭ Vol. 40; no. 3; pp. 185 - 192 |
|---|---|
| Main Authors | , , , , , , |
| Format | Journal Article |
| Language | Chinese |
| Published |
Beijing
Marine Geology and Quaternary Geology
01.01.2020
浙江师范大学地理与环境科学学院,金华,321004 |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0256-1492 |
| DOI | 10.16562/j.cnki.0256-1492.2019120501 |
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| Abstract | 根据黄土高原中东部地区黄土沉积物的地质记录，前人研究推断MIS13时期北半球气候为高温高湿环境，然而，这似乎与黄土高原西部黄土沉积物的地质记录存在差别。本研究通过综合前人的研究结果，对比黄土高原东西部地区MIS13时期的古气候及古土壤风化强度在空间上的梯度分布，发现两地的古气候演化存在不对称性。对比MIS13时期低纬度的亚非季风区和北半球中高纬度地区气候状况得出：高降水量环境仅存在于亚非季风区大部分地区，但当时是否呈现高温环境值得商榷；北半球中高纬地区则显著不同，呈现相对较干冷的间冰期气候。由此推断，MIS13时期黄土高原东西部地区之间气候演化的不对称现象可能是季风缺少动力因素，对黄土高原西部影响较小，且长时间停留在黄土高原中东部地区所致；而在此之后的间冰期，由于季风的扩展和加深可能进一步加剧黄土高原西部地区S5S1古土壤风化强度与年轻古土壤层的差别。 |
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| AbstractList | 根据黄土高原中东部地区黄土沉积物的地质记录，前人研究推断MIS13时期北半球气候为高温高湿环境，然而，这似乎与黄土高原西部黄土沉积物的地质记录存在差别。本研究通过综合前人的研究结果，对比黄土高原东西部地区MIS13时期的古气候及古土壤风化强度在空间上的梯度分布，发现两地的古气候演化存在不对称性。对比MIS13时期低纬度的亚非季风区和北半球中高纬度地区气候状况得出：高降水量环境仅存在于亚非季风区大部分地区，但当时是否呈现高温环境值得商榷；北半球中高纬地区则显著不同，呈现相对较干冷的间冰期气候。由此推断，MIS13时期黄土高原东西部地区之间气候演化的不对称现象可能是季风缺少动力因素，对黄土高原西部影响较小，且长时间停留在黄土高原中东部地区所致；而在此之后的间冰期，由于季风的扩展和加深可能进一步加剧黄土高原西部地区S5S1古土壤风化强度与年轻古土壤层的差别。 P532; 根据黄土高原中东部地区黄土沉积物的地质记录,前人研究推断MIS13时期北半球气候为高温高湿环境,然而,这似乎与黄土高原西部黄土沉积物的地质记录存在差别.本研究通过综合前人的研究结果,对比黄土高原东西部地区MIS13时期的古气候及古土壤风化强度在空间上的梯度分布,发现两地的古气候演化存在不对称性.对比MIS13时期低纬度的亚非季风区和北半球中高纬度地区气候状况得出:高降水量环境仅存在于亚非季风区大部分地区,但当时是否呈现高温环境值得商榷;北半球中高纬地区则显著不同,呈现相对较干冷的间冰期气候.由此推断,MIS13时期黄土高原东西部地区之间气候演化的不对称现象可能是季风缺少动力因素,对黄土高原西部影响较小,且长时间停留在黄土高原中东部地区所致;而在此之后的间冰期,由于季风的扩展和加深可能进一步加剧黄土高原西部地区S5S1古土壤风化强度与年轻古土壤层的差别. |
| Author | LI, Fengquan WANG, Bo WANG Niuniu Qu, CHEN YANG, Liwen WANG, Zhiyuan ZHANG Xingze |
| AuthorAffiliation | 浙江师范大学地理与环境科学学院,金华,321004 |
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| DOI | 10.16562/j.cnki.0256-1492.2019120501 |
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| Snippet | 根据黄土高原中东部地区黄土沉积物的地质记录，前人研究推断MIS13时期北半球气候为高温高湿环境，然而，这似乎与黄土高原西部黄土沉积物的地质记录存在差别。本研究通过综... P532; 根据黄土高原中东部地区黄土沉积物的地质记录,前人研究推断MIS13时期北半球气候为高温高湿环境,然而,这似乎与黄土高原西部黄土沉积物的地质记录存在差别.本研究通过... |
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| SubjectTerms | Archives & records Climate Geochemistry Geophysics Humid climates Isotopes Loess Mineralogy Monsoons Paleoclimate science Paleosols Precipitation Quaternary Science Soils Wind |
| Title | MIS13时期黄土高原东西部地区夏季风不对称演化 |
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