Holocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman

By D. Fleitmann, S. Burns, Manfred Mudelsee, U. Neff, J. Kramers, A. Mangini, A. Matter. Science, 2003

1,673 citations recorded by the source corpus.

Subfields: Anthropology, Atmospheric Science, Earth-Surface Processes

View Paper: https://www.semanticscholar.org/paper/94b479a51b7469e2520a9015008e799acee89377

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Anthropology

1. R. Muscheler
2. K. Kodera

In Atmospheric Science

1. M. Lockwood
2. J. Haigh
3. M. Vonmoos
4. R. Muscheler
5. K. Matthes
6. L. Gray
7. J. Beer
8. K. Kodera

In Earth-Surface Processes

1. K. Kodera

Citations in the corpus

• SOLAR INFLUENCES ON CLIMATE (2010, positive): “The d18O from a stalagmite in Oman (Figure 19, bottom) is mainly a proxy for the amount of monsoon precipitation [Fleitmann et al., 2003].”
• Climate change and solar variability: what's new under the sun? (2006, background): “The search for solar variability in climate records spanning the Holocene has been revived recently by analyzing O/O fluctuations, a proxy for rainfall, in well-dated speleothems from the Asian monsoon area [59–61].”
• Solar influence on the Indian Ocean Monsoon through dynamical processes (2004, methodology): “Recent advances in reconstruction of the past climate with fine temporal resolution clarified the relationship between the solar cycles and the monsoon rainfall in South Oman with multiple time scales from decadal to millennial [Neff et al., 2001; Burns et al., 2002; Fleitmann et al., 2003 ].”
• Large variations in Holocene solar activity: Constraints from 10Be in the Greenland Ice Core Project ice core (2006, background): “There is a growing number of paleoclimatic studies pointing toward a strong solar forcing on past climate [Bond et al., 2001; Denton and Karle´n, 1973; Fleitmann et al., 2003; Hodell et al., 2001; Magny, 1993; Neff et al., 2001; Van Geel et al., 1996; Verschuren et al., 2000].”
• “Amount effect” of water isotopes and quantitative analysis of post‐condensation processes (2008, methodology): “This relationship, called the “amount effect”, has been used to estimate past storm activity derived from paleoproxies such as speleothems that record the isotopic history in precipitation ( Fleitmann et al., 2003 ).”