A Brief Commentary on the Interpretation of Chinese Speleothem δ18O Records as Summer Monsoon Intensity Tracers

AbstractWe present a new set of clay mineral and grain-size data for the siliciclastic sediment fraction from International Ocean Discovery Program (IODP) Site U1456 located in the eastern Arabian Sea to reconstruct the variabilities in the continental erosion and weathering intensity in the western Himalaya, elucidate the sediment source-to-sink processes and discuss the potential controls underlying these changes since 3.7 Ma. The clay minerals mainly consist of smectite (0–90%, average 44%) and illite (3–90%, average 44%), with chlorite (1–26%, average 7%) and kaolinite (0–19%, average 5%) as minor components. The compositional variations in the clay minerals at IODP Site U1456 suggest four phases of sediment provenance: the Indus River (phase 1, 3.7–3.2 Ma), the Indus River and Deccan Traps (phase 2, 3.2–2.6 Ma), the Indus River (phase 3, 2.6–1.2 Ma) and the Indus River and Deccan Traps (phase 4, 1.2–0 Ma). These provenance changes since 3.7 Ma can be correlated with variations in the Indian summer monsoon intensity. The siliciclastic sediments in the eastern Arabian Sea were mainly derived from the Indus River when the Indian summer monsoon was generally weak. In contrast, when the Indian summer monsoon intensified, the siliciclastic sediment supply from the Deccan Traps increased. In particular, this study shows that the smectite/(illite+chlorite) ratio is a sensitive tool for reconstructing the history of the variation in the Indian summer monsoon intensity over the continents surrounding the Arabian Sea since 3.7 Ma.

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East Asian summer monsoon intensity inferred from iron oxide mineralogy in the Xiashu Loess in southern China

Quaternary Science Reviews ◽

10.1016/j.quascirev.2008.10.002 ◽

2009 ◽

Vol 28 (3-4) ◽

pp. 345-353 ◽

Cited By ~ 34

Author(s):

Weiguo Zhang ◽

Lizhong Yu ◽

Min Lu ◽

Xiangmin Zheng ◽

Junfeng Ji ◽

...

Keyword(s):

Iron Oxide ◽

Summer Monsoon ◽

East Asian Summer Monsoon ◽

Southern China ◽

Asian Summer Monsoon ◽

East Asian ◽

Monsoon Intensity ◽

Asian Summer

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Variation in the Asian monsoon intensity and dry–wet conditions since the Little Ice Age in central China revealed by an aragonite stalagmite

Climate of the Past ◽

10.5194/cp-10-1803-2014 ◽

2014 ◽

Vol 10 (5) ◽

pp. 1803-1816 ◽

Cited By ~ 15

Author(s):

J.-J. Yin ◽

D.-X. Yuan ◽

H.-C. Li ◽

H. Cheng ◽

T.-Y. Li ◽

...

Keyword(s):

Summer Monsoon ◽

El Niño ◽

El Nino ◽

Asian Summer Monsoon ◽

Eastern China ◽

Central China ◽

Solar Irradiation ◽

Mountain Area ◽

Monsoon Intensity ◽

Asian Summer

Abstract. This paper focuses on the climate variability in central China since AD 1300, involving: (1) a well-dated, 1.5-year resolution stalagmite δ18O record from Lianhua Cave, central China (2) links of the δ18O record with regional dry–wet conditions, monsoon intensity, and temperature over eastern China (3) correlations among drought events in the Lianhua record, solar irradiation, and ENSO (El Niño–Southern Oscillation) variation. We present a highly precise, 230Th / U-dated, 1.5-year resolution δ18O record of an aragonite stalagmite (LHD1) collected from Lianhua Cave in the Wuling Mountain area of central China. The comparison of the δ18O record with the local instrumental record and historical documents indicates that (1) the stalagmite δ18O record reveals variations in the summer monsoon intensity and dry–wet conditions in the Wuling Mountain area. (2) A stronger East Asian summer monsoon (EASM) enhances the tropical monsoon trough controlled by ITCZ (Intertropical Convergence Zone), which produces higher spring quarter rainfall and isotopically light monsoonal moisture in the central China. (3) The summer quarter/spring quarter rainfall ratio in central China can be a potential indicator of the EASM strength: a lower ratio corresponds to stronger EASM and higher spring rainfall. The ratio changed from <1 to >1 after 1950, reflecting that the summer quarter rainfall of the study area became dominant under stronger influence of the Northwestern Pacific High. Eastern China temperatures varied with the solar activity, showing higher temperatures under stronger solar irradiation, which produced stronger summer monsoons. During Maunder, Dalton and 1900 sunspot minima, more severe drought events occurred, indicating a weakening of the summer monsoon when solar activity decreased on decadal timescales. On an interannual timescale, dry conditions in the study area prevailed under El Niño conditions, which is also supported by the spectrum analysis. Hence, our record illustrates the linkage of Asian summer monsoon precipitation to solar irradiation and ENSO: wetter conditions in the study area under stronger summer monsoon during warm periods, and vice versa. During cold periods, the Walker Circulation will shift toward the central Pacific under El Niño conditions, resulting in a further weakening of Asian summer monsoons.

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A Moments View of Climatology and Variability of the Asian Summer Monsoon Anticyclone

Journal of Climate ◽

10.1175/jcli-d-20-0729.1 ◽

2021 ◽

pp. 1-69

Author(s):

Gloria L Manney ◽

Michelle L Santee ◽

Zachary D Lawrence ◽

Krzysztof Wargan ◽

Michael J Schwartz

Keyword(s):

Aspect Ratio ◽

Interannual Variability ◽

Summer Monsoon ◽

Asian Summer Monsoon ◽

Major Axis ◽

Subtropical Jet ◽

Monsoon Intensity ◽

Typical Aspect ◽

Asian Summer ◽

New Evidence

AbstractA comprehensive investigation of the climatology of and interannual variability and trends in the Asian summer monsoon anticyclone (ASMA) is presented, based on a novel area and moments analysis. Moments include centroid location, aspect ratio, angle, and “excess kurtosis” (measuring how far the shape is from elliptical) for an equivalent ellipse with the same area as the ASMA. Key results are robust among the three modern reanalyses studied. The climatological ASMA is nearly elliptical, with its major axis aligned along its centroid latitude and a typical aspect ratio of ~5–8. The ASMA centroid shifts northward with height, northward and westward during development, and in the opposite direction as it weakens. New evidence finding no obvious climatological bimodality in the ASMA reinforces similar suggestions from previous studies using modern reanalyses. Most trends in ASMA moments are not statistically significant. ASMA area and duration, however, increased significantly during 1979–2018; the 1958–2018 record analyzed for one reanalysis suggests that these trends may have accelerated in recent decades. ASMA centroid latitude is significantly positively (negatively) correlated with subtropical jet core latitude (altitude), and significantly negatively correlated with concurrent ENSO; these results are consistent with and extend previous work relating monsoon intensity, ENSO, and jet shifts. ASMA area is significantly positively correlated with the MEI ENSO index two months previously. These results improve our understanding of the ASMA using consistently defined diagnostics of its size, geometry, interannual variability, and trends that have not previously been analyzed.

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TRACKING CHANGES IN INDIAN SUMMER MONSOON INTENSITY USING PRECIPITATION AND LAKE LEVEL PROXIES FROM EASTERN TIBET

10.1130/abs/2017ne-290151 ◽

2017 ◽

Author(s):

Melanie Perello ◽

◽

Broxton W. Bird ◽

Yanbin Lei ◽

Pratigya J. Polissar ◽

...

Keyword(s):

Summer Monsoon ◽

Indian Summer Monsoon ◽

Lake Level ◽

Eastern Tibet ◽

Monsoon Intensity

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Multi‐Centennial‐Scale Variations of South American Summer Monsoon Intensity in the Southern Central Andes (24–27°S) During the Late Holocene

Geophysical Research Letters ◽

10.1029/2019gl084157 ◽

2020 ◽

Vol 47 (4) ◽

Cited By ~ 2

Author(s):

Sebastian T. Kock ◽

Karsten Schittek ◽

Bertil Mächtle ◽

Antonio Maldonado ◽

Heinz Vos ◽

...

Keyword(s):

Summer Monsoon ◽

Late Holocene ◽

Central Andes ◽

South American ◽

Monsoon Intensity ◽

Southern Central

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Precipitation variations of Longxi, northeast margin of Tibetan Plateau since AD 960 and their relationship with solar activity

Climate of the Past ◽

10.5194/cp-4-19-2008 ◽

2008 ◽

Vol 4 (1) ◽

pp. 19-28 ◽

Cited By ~ 63

Author(s):

◽

Keyword(s):

Solar Activity ◽

Tibetan Plateau ◽

Northern Hemisphere ◽

Summer Monsoon ◽

Early Years ◽

Last Millennium ◽

Northern Hemisphere Temperature ◽

Hemisphere Temperature ◽

Monsoon Intensity ◽

North Edge

Abstract. The precipitation variations of Longxi area, northeast margin of the Tibetan Plateau since AD 960 are reconstructed from Chinese historical documentary records. These records show that since AD 960, the precipitation of Longxi decreased and reached the lowest level at the end of the 17th and the 18th centuries. After this period, the precipitation gradually increased. The three short wet periods of Longxi in the last millennium were: from the end of the 10th century to the early years of the 11th century, from the end of the 12th century to the early years of the 13th century and during the first half of the 20th century. The precipitation variations coincide well with variations of the Northern Hemisphere temperature and the atmospheric 14C concentration, as well as the averaged 10Be concentration and the reconstructed solar modulation record which show that solar activity may be an important driving force of the precipitation variations of Longxi on multi-decadal to centennial scales during the last millennium. Solar activity controls the motion of the north edge of the Asian summer monsoon by affecting the Asia summer monsoon intensity, the East Asian winter monsoon intensity and the locations of westerlies, thus further dominating precipitation variations of Longxi. Synchronous variations of Longxi precipitation and Northern Hemisphere temperature may also be ascribed to the same control of solar activity.

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