东亚季风

  • 网络East Asian monsoon;EASM
东亚季风东亚季风
  1. 在不同的SST年代际背景下,东亚季风和ENSO事件的关系是不同的。

    The relationship between the east Asian monsoon ( EAM ) and ENSO events is different on the different interdecadal background in SST fields .

  2. 运用小波分析方法和相关分析对东亚季风的准两年振荡(QBO)的存在及其与ENSO变率的关系进行了研究。

    In the context of wavelet technique and coherence analysis the existence of east Asian monsoon QBO is investigated together with its relation to ENSO variability .

  3. ENSO对我国东亚季风和我国气候影响;

    The effect of ENSO on Eastern Asian monsoon and climate of China ;

  4. ENSO对其后东亚季风活动影响的GCM模拟研究

    Numerical simulation of the ENSO influences on East-Asian monsoon activities afterwards

  5. YoungerDryas时期东亚季风气候和中国东部沙区沙漠变化

    Monsoon climate in East Asia and desert change in eastern China during Younger Dryas period

  6. 东亚季风和南亚季风的反相位关系及其与ENSO的联系:年际尺度和轨道尺度

    Inverse phase between South Asian and East Asian summer monsoons and its relation with enso : from interannual to orbital scale

  7. 东亚季风的QBO促使ENSO循环表现出显著的季节锁相,并维持了ENSO事件的一年左右的暖相位。

    The monsoon QBO is responsible for strong seasonal ENSO phase locking and for its warm phase lasting one year or so .

  8. 这个新的东亚季风指数基本上满足了由Lau等提出的最佳季风指数的原则。

    In comparison with other indices , the new index is basically satisfied with the optimal principles for monsoon indices proposed by Lau et al .

  9. 区域气候模式REMO对东亚季风季节变化的模拟研究

    Simulation of Monsoon Seasonal Variation of Regional Climate Model REMO in East Asia

  10. 结果表明,由于SSTA在大气中强迫激发出了大气低频振荡,使得ENSO对其后的东亚季风活动仍有明显影响。

    The results show that the influences of ENSO on the afterward monsoon activities in East Asia are in existance owing to atmospheric low frequency oscillation excited by SSTA .

  11. 夏季东亚季风区500hPa月环流异常及其与我国降水关系的向量EOF分析

    Vector EOF Expansion of Summer Monthly Anomalous Wind Fields at 500 hPa over East Asia Relation to Rainfall over China

  12. 同时由于北半球冰盖及末次冰期较低的大气CO2浓度的影响,也有效地延迟了东亚季风的加强,但是这些因素对西南季风却没有很大影响。

    And possibly the remnant Northern Hemisphere ice sheets and the lowered concentration of carbon dioxide in the atmosphere during the last glaciation that delayed the development of the East Asian monsoon , but had less influence on the tropical Indian monsoon .

  13. PDO和伴随的亚非大陆和印度洋地区之间海陆热力差异的年代际变化对印度洋海温和东亚季风降水年际联系具有明显的调节作用。

    The interannual relationship between Indian Ocean SST and East Asia monsoon rainfall is regulated by the PDO associated with interdecadal variations of land-sea thermodynamic defference between Asia-Africa continent and Indian Ocean .

  14. 指出了青藏高原感热驱动气泵(SHAP)在调制东亚季风及全球气候中的重要作用;

    The importance of the Sensible Heat driven Air Pump ( SHAP ) over the Qinghai Xizang Plateau in regulating the East Asian monsoons and global climate is emphasized .

  15. 中全新世相应时段两支石笋δ~(18)O序列与树轮△~(14)C(res)曲线的良好对应关系说明了东亚季风降水波动在百年~十年尺度上显著受太阳驱动。

    The good corresponding between the two stalagmites δ ~ 18O time series and tree ring Δ ~ 14C_res curve during the counterpart periods of mid-Holocene suggests that the precipitation change of East Asian monsoon is markedly driven by the solar activity at the centennial - to decadal-scale .

  16. 利用中科院大气所的IAPAGCM-Ⅱ大气环流模式,模拟了在存在和没有赤道东太平洋海温异常影响下,印度洋偶极子对东亚季风区天气气候的影响。

    This paper analyses the Indian Ocean Dipole ( IOD ) influence on climate variations over East Asian monsoon region , based on CAS 's IAP AGCM - ⅱ with Equator East Pacific SSTA influence on or not .

  17. 北太平洋中、西部副高在北进期的脊线活动均存在显著的10~20d周期低频振荡,东亚季风区还具有明显的准40d振荡周期。

    The ridge movement has 10 ~ 20-day low-frequency oscillation during its northward over central and western Pacific , particularly in East-Asian monsoon area with quasi-40-day oscillation period .

  18. 福建晋江科任(KR)老红砂分布区地处我国东南沿海,属于东亚季风影响的典型区域,较好的记录了东亚季风控制区古气候演变过程。

    The distribution area of KR " old red sand " of Jinjiang in Fujian locating in the southeast coast of China is the typical region strongly influenced by the East Asian monsoon which can nicely record the paleoclimate evolutionary process of the East Asian monsoon .

  19. 东亚季风强度变化对河北省气候的影响

    Influence of East-Asia Monsoon Intensity Change on Climate in Hebei Province

  20. 孟加拉湾深对流加热对东亚季风环流系统的影响

    Effect of Bob deep convection heating on East Asian monsoon circulation

  21. 东亚季风区夏季风强度和降水的配置关系

    The Configurable Relationships between Summer Monsoon and Precipitation over East Asia

  22. 东亚季风研究取得重要成果

    Significant progress in the research of the East Asian monsoon

  23. 1994年6月东亚季风异常的数值模拟

    Numerical simulation of Abnormal East Asia monsoon in June 1994

  24. 东亚季风区植被-大气相互作用研究;

    Study of vegetation-climate interaction in East Asia Monsoon region ;

  25. 东亚季风对西北地区干旱气候的影响

    Effect of East - Asian Monsoon on Drought Climate of Northwest China

  26. 东亚季风边缘带上的植被变化

    Vegetation variations along the monsoon boundary zone in East Asia

  27. 倒数第二次冰期晚期东亚季风气候演变的石笋δ~(18)O记录

    East Asian monsoon climate during the late Penultimate Glaciation based on stalagmite records

  28. 东亚季风区的极端气候事件及其原因

    Pleistocene climate extremes in East Asia and their causes

  29. 末次间冰期东亚季风百年&十年际分辨率洞穴石笋记录

    Decadal-to Century-scale High Resolution Stalagmites Record of Asian Monsoon during the Last Interglacial

  30. 东亚季风边缘活动带研究综述

    Research on East Asian Summer Monsoon : A Review