• No results found

[PDF] Top 20 Precipitation record since AD 1600 from ice cores on the central Tibetan Plateau

Has 10000 "Precipitation record since AD 1600 from ice cores on the central Tibetan Plateau" found on our website. Below are the top 20 most common "Precipitation record since AD 1600 from ice cores on the central Tibetan Plateau".

Precipitation record since AD 1600 from ice cores on the central Tibetan Plateau

Precipitation record since AD 1600 from ice cores on the central Tibetan Plateau

... high precipitation throughout the entire 20th century, similar to that in the 18th century, during a time of gradual global ...and precipitation con- trasts with snow accumulation record from ... See full document

6

A 70-yr record of oxygen-18 variability in an ice core from the Tanggula Mountains, central Tibetan Plateau

A 70-yr record of oxygen-18 variability in an ice core from the Tanggula Mountains, central Tibetan Plateau

... m ice core was retrieved from the Tanggula Mts, central Tibetan Plateau at 5743 m ...series since the mid-1930s. Data are compared to previous results of an ice core ... See full document

9

Significant recent warming over the northern Tibetan Plateau from ice core 18 O records

Significant recent warming over the northern Tibetan Plateau from ice core 18 O records

... O record may be attributed to the different seasonal moisture sources in this ...in precipitation. On the other hand, precipitation δ 18 O in the monsoon season could be af- fected by a variety of ... See full document

11

Large-scale atmospheric forcing and topographic modification of precipitation rates over High Asia – a neural-network-based approach

Large-scale atmospheric forcing and topographic modification of precipitation rates over High Asia – a neural-network-based approach

... derived from near-surface meteorologi- cal records (Bao and Zhang, 2012) and radiosonde observa- tions over the Tibetan Plateau (Wang and Zeng, 2012) and the central Himalayan Arc (Jin-Huan et ... See full document

21

Influence of regional precipitation patterns on stable isotopes in ice cores from the central Himalayas

Influence of regional precipitation patterns on stable isotopes in ice cores from the central Himalayas

... reveal precipitation seasonality along the Himalayas, monthly precipitation amount data from four Himalayan me- teorological stations (Pali, Dingri, Nyalam, and Pulan sta- tions; ...available ... See full document

13

Differences in the water balance components of four lakes in the  southern central Tibetan Plateau

Differences in the water balance components of four lakes in the southern central Tibetan Plateau

... the Tibetan Plateau (TP) are indicators of differences in the water balance over the ...higher precipitation totals and attributed runoff generation in the Nam Co and Tangra Yumco ...basins. ... See full document

17

Recent mass balance of the Purogangri Ice Cap, central Tibetan Plateau, by means of differential X-band SAR interferometry

Recent mass balance of the Purogangri Ice Cap, central Tibetan Plateau, by means of differential X-band SAR interferometry

... data from February 2000 and compared it with TSX/TDX data acquired in January 2012 following two dif- ferent ...the ice cap while rapid negative elevation changes were found in glacier tongue ...estimated ... See full document

11

Age ranges of the Tibetan ice cores with emphasis on the Chongce ice cores, western Kunlun Mountains

Age ranges of the Tibetan ice cores with emphasis on the Chongce ice cores, western Kunlun Mountains

... of ice core records. However, dat- ing ice cores drilled from the high-elevation glaciers is chal- lenging and often problematic, leading to great uncertain- ...Guliya ice core, drilled ... See full document

8

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

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

... starts from AD 960, with the scarcity of historical records in the early years, we first classify the records to 5 levels year by year as D/F index, using traditional classification ...1983). Since ... See full document

10

Strong summer monsoon during the cool MIS-13

Strong summer monsoon during the cool MIS-13

... deep-sea cores from different ...EPICA ice core through the so-called “see-saw” argument (Stocker and Johnsen, 2003): stronger NADW would indeed bring more heat from the equator and the ... See full document

6

Rapid wastage of the Hazen Plateau ice caps, northeastern Ellesmere Island, Nunavut, Canada

Rapid wastage of the Hazen Plateau ice caps, northeastern Ellesmere Island, Nunavut, Canada

... Hazen Plateau of northeastern Ellesmere Island, Nunavut, Canada, is a rolling upland, with elevations rising from about 300 m above sea level ...The plateau is unglaciated with the exception of two ... See full document

9

Was the 4 2 ka Event an Anthropogenic Disaster?

Was the 4 2 ka Event an Anthropogenic Disaster?

... the Tibetan Plateau during HCO was more humid than it is now [40] [70]-[73] due to 1) an increased precipitation carried by the western circulation, 2) di- rection of the Indian monsoon to western ... See full document

19

An assessment of the impact of ATMS and CrIS data assimilation on precipitation prediction over the Tibetan Plateau

An assessment of the impact of ATMS and CrIS data assimilation on precipitation prediction over the Tibetan Plateau

... maximum precipitation always occurred at 18:00–21:00 UTC (00:00–03:00 ...away from the measured values due to an inac- curate initial ...data from the DA experiments are closer to the observations ... See full document

15

Trends in flood seasonality of the River Ouse (Northern England) from archive and instrumental sources since AD 1600

Trends in flood seasonality of the River Ouse (Northern England) from archive and instrumental sources since AD 1600

... The principal finding of this work has been the shift in flood seasonality within the period AD 1800-1999 from the December-January to the February-March bi-monthly period, particularly for high flows ... See full document

39

Modeling sensitivity study of the possible impact of snow and glaciers developing over Tibetan Plateau on Holocene African-Asian summer monsoon climate

Modeling sensitivity study of the possible impact of snow and glaciers developing over Tibetan Plateau on Holocene African-Asian summer monsoon climate

... and precipitation fields) is used to simulate temporal dynamics of vegetation cover and in turn, the vegetation cover and the maximum of LAI are accounted for in calculating the surface albedo, roughness, and ... See full document

13

Archival processes of the water stable isotope signal in East Antarctic ice cores

Archival processes of the water stable isotope signal in East Antarctic ice cores

... positions contrasting with results from NEEM and Kohnen (Steen-Larsen et al., 2014; Ritter et al., 2016). Our obser- vations are largely consistent with a closed system: during frost events, the vapour becomes ... See full document

22

Analysis of Extreme Precipitation Events over Central Plateau of Iran

Analysis of Extreme Precipitation Events over Central Plateau of Iran

... mainly from Persian Gulf over the past three days (72-h) till the peak time of system’s activity over the study area Figure ...came from Red Sea towards the central regions of Iran Figure ... See full document

17

The GAMDAM glacier inventory: a quality-controlled inventory of Asian glaciers

The GAMDAM glacier inventory: a quality-controlled inventory of Asian glaciers

... Discharge from the Asian Mountains” ...sets from the period 1999–2003, in con- junction with a digital elevation model (DEM) and high- resolution Google Earth TM ... See full document

16

Temperature and precipitation signal in two Alpine ice cores over the period 1961–2001

Temperature and precipitation signal in two Alpine ice cores over the period 1961–2001

... temperature from the Twentieth Century Reanalysis data set (Compo et ...region from 40 ◦ to 60 ◦ N and from 15 ◦ W to 25 ◦ E. For precipitation, because of its sporadic nature in space and ... See full document

16

Holocene vegetation and biomass changes on the Tibetan Plateau – a model-pollen data comparison

Holocene vegetation and biomass changes on the Tibetan Plateau – a model-pollen data comparison

... northern Tibetan Plateau (see ...arise from a lower (pre-industrial) greenhouse-gas concentra- tion in the ...Global Precipitation Clima- tology Project (GPCP); Adler et ...the central ... See full document

21

Show all 10000 documents...