Sentences with phrase «asian summer monsoon»

In summary, an intensification of the Asian summer monsoon and an enhancement of summer monsoon precipitation variability with increased greenhouse gases that was reported in the SAR has been corroborated by new studies.

«The South Asian summer monsoon directly affects the lives of more than 1 / 6th of the world's population.

Seasonal forecasting of East Asian summer monsoon based on oceanic heat sources.

Lee, E., T. N. Chase, and B. Rajagopalan, Highly improved predictive skill in the forecasting of the northern East Asian summer monsoon, Water Resources Research (In Press)

Lee Eungul, Thomas N. Chase, Peter J. Lawrence, Balaji Rajagopalan, Model assessment of the observed relationjship between El Nino and the northern East Asian summer monsoon using the CCSM3, J. Geophys.

Lee Eungul, Thomas N. Chase, Peter J. Lawrence, Balaji Rajagopalan, Model assessment of the observed relationship between El Nino and the northern East Asian summer monsoon using the CCSM3, J. Geophys.

Lee, E., T. N. Chase, and B. Rajagopalan, Highly improved predictive skill in the forecasting of the northern East Asian summer monsoon, Water Resources Research, 44, W10422, doi: 10.1029 / 2007WR006514

Lin J. L., K. M. Weickmann, G. N. Kiladis, B. E. Mapes, et al. (September 2008): Subseasonal Variability Associated with Asian Summer Monsoon Simulated by 14 IPCC AR4 Coupled GCMs.

Shin, Z. Liu and Q. Liu (October 2016): Sensitivity of Asian Summer Monsoon precipitation to tropical sea surface temperature anomalies.

It can also strengthen the Asian summer monsoon circulation and cause a local increase in precipitation, despite the global reduction of evaporation that compensates aerosol radiative heating at the surface (Miller et al., 2004b).

The fourth assessment report of the IPCC had this to say about the monsoon: «It is likely that warming associated with increasing greenhouse gas concentrations will cause an increase of Asian summer monsoon precipitation variability.

Using eight AOGCMs, Ueda et al. (2006) demonstrate that pronounced warming over the tropics results in a weakening of the Asian summer monsoon circulations in relation to a reduction in the meridional thermal gradients between the Asian continent and adjacent oceans.

However, at the start of Bond events, which are smaller and briefer than Heinrich events, the Asian summer monsoon weakened more gradually, taking about 110 years to reach its weakest point.

Increased southern East Asian summer monsoon (SEASM) precipitation is related to warm WNP SST anomalies which create a weaker WNP anticyclone.

More recently we have examined the East Asian summer monsoon (EASM) system and found that it is physically two distinct systems with a northern and southern component driven by distinct forcing mechanisms.

For example, the northern East Asian summer monsoon (NEASM) is, for the years of highest SST anomalies in the tropical eastern Pacific (TEP), affected by the Pacific - East Asian (PEA) teleconnection pattern, which consists of a wave creating an anomalously strong western North Pacific (WNP) anticyclonic circulation and anomalously strong cyclonic circulation in the NEASM region, creating more monsoon rainfall.

Influence of the land surface in the Asian summer monsoon: External conditions versus internal feedbacks

Variability in climatology and agricultural production in China in association with the East Asian summer monsoon and El Nio Southern Oscillation

Li, H., Dai, A., Zhou, T. & Lu, J. Responses of East Asian summer monsoon to historical SST and atmospheric forcing during 1950 — 2000.

Some studies suggest that climate change may be one of the reasons that the Asian Summer Monsoon weakened.

Since El Nino also has an important impact on the Asian Summer Monsoon in particular, its hard to know precisely what large - scale changes in atmospheric circulation are due to the radiative forcing of the eruption itself, and the secondary response to that eruption of ENSO.

The East Asian summer monsoon and desertification in Eurasia is driven by fluctuating Northern Hemisphere ice volume and global sea level during the Ice Age, as shown in a study published in Nature Communications.

Annamalai, H., K. Hamilton, and K.R. Sperber, 2007: South Asian summer monsoon and its relationship with ENSO in the IPCC AR4 simulations.

The broad comparability between the HML paleo - proxies, Chinese speleothem δ18Orecords, and the northern hemisphere summer insolation throughout the Holocene, suggests that solar insolation exerts a profound influence on ASM [Asian summer monsoon] changes.

Based on a summer monsoon index derived from MSLP gradients between land and ocean in the East Asian region, Guo et al. (2003) found a systematic reduction in the East Asian summer monsoon during 1951 to 2000, with a stronger monsoon dominant in the first half of the period and a weaker monsoon prevailing in the second half (Figure 3.35).

Not exact matches

This summer, scientists produced a report finding that the monsoon amounted to an «efficient smokestack» for Asian pollution, spreading it «throughout the entire Northern Hemisphere.»

He has created computer simulations indicating that sulfate clouds could potentially weaken the Asian and African summer monsoons, reducing rain that irrigates the food crops of billions of people.

The other (much smaller) major pathway for transporting air from the lower atmosphere to the stratosphere is the Asian monsoon circulation, which prevails in the summer.

This long - term change in the East Asian monsoon index is consistent with a tendency for a southward shift of the summer rain belt over eastern China (Zhai et al., 2004).

During summer, the Asian Monsoon is not only important for Asia but affects weather patterns over the entire northern hemisphere.

In the tropics, an increase in precipitation is projected by the end of the 21st century in the Asian monsoon and the southern part of the West African monsoon with some decreases in the Sahel in northern summer (Cook and Vizy, 2006), as well as increases in the Australian monsoon in southern summer in a warmer climate (Figure 10.9).

This is the regime of the monsoon (rain - bearing winds), which is associated with the heating of the Asian landmass in summer and its intense cooling in winter.

In early summer a second failure of the Indian monsoon unleashes panic in the rice market, where Asian households have been steadily hoarding.