Precipitation variability in the Indian Central Himalaya during last ca. 4,000 years inferred from a speleothem record: Impact of Indian Summer Monsoon (ISM) and Westerlies
We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipita...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kotlia, Bahadur Singh [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015transfer abstract |
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| Schlagwörter: |
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| Umfang: |
10 |
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| Übergeordnetes Werk: |
Enthalten in: Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids - Xiao, Qiuyun ELSEVIER, 2021, the journal of the International Union for Quaternary Research, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:371 ; year:2015 ; day:12 ; month:06 ; pages:244-253 ; extent:10 |
| Links: |
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| DOI / URN: |
10.1016/j.quaint.2014.10.066 |
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ELV03472088X |
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| 245 | 1 | 0 | |a Precipitation variability in the Indian Central Himalaya during last ca. 4,000 years inferred from a speleothem record: Impact of Indian Summer Monsoon (ISM) and Westerlies |
| 264 | 1 | |c 2015transfer abstract | |
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| 520 | |a We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. | ||
| 520 | |a We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. | ||
| 650 | 7 | |a Late Holocene |2 Elsevier | |
| 650 | 7 | |a Oxygen and carbon isotopes |2 Elsevier | |
| 650 | 7 | |a Stalagmite |2 Elsevier | |
| 650 | 7 | |a Westerlies |2 Elsevier | |
| 650 | 7 | |a Indian Central Himalaya |2 Elsevier | |
| 650 | 7 | |a Indian Summer Monsoon (ISM) |2 Elsevier | |
| 700 | 1 | |a Singh, Anoop Kumar |4 oth | |
| 700 | 1 | |a Joshi, Lalit Mohan |4 oth | |
| 700 | 1 | |a Dhaila, Bachi Singh |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Xiao, Qiuyun ELSEVIER |t Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids |d 2021 |d the journal of the International Union for Quaternary Research |g Amsterdam [u.a.] |w (DE-627)ELV005958261 |
| 773 | 1 | 8 | |g volume:371 |g year:2015 |g day:12 |g month:06 |g pages:244-253 |g extent:10 |
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10.1016/j.quaint.2014.10.066 doi GBVA2015017000004.pica (DE-627)ELV03472088X (ELSEVIER)S1040-6182(14)00831-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Kotlia, Bahadur Singh verfasserin aut Precipitation variability in the Indian Central Himalaya during last ca. 4,000 years inferred from a speleothem record: Impact of Indian Summer Monsoon (ISM) and Westerlies 2015transfer abstract 10 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. Late Holocene Elsevier Oxygen and carbon isotopes Elsevier Stalagmite Elsevier Westerlies Elsevier Indian Central Himalaya Elsevier Indian Summer Monsoon (ISM) Elsevier Singh, Anoop Kumar oth Joshi, Lalit Mohan oth Dhaila, Bachi Singh oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:371 year:2015 day:12 month:06 pages:244-253 extent:10 https://doi.org/10.1016/j.quaint.2014.10.066 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 371 2015 12 0612 244-253 10 045F 550 |
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10.1016/j.quaint.2014.10.066 doi GBVA2015017000004.pica (DE-627)ELV03472088X (ELSEVIER)S1040-6182(14)00831-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Kotlia, Bahadur Singh verfasserin aut Precipitation variability in the Indian Central Himalaya during last ca. 4,000 years inferred from a speleothem record: Impact of Indian Summer Monsoon (ISM) and Westerlies 2015transfer abstract 10 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. Late Holocene Elsevier Oxygen and carbon isotopes Elsevier Stalagmite Elsevier Westerlies Elsevier Indian Central Himalaya Elsevier Indian Summer Monsoon (ISM) Elsevier Singh, Anoop Kumar oth Joshi, Lalit Mohan oth Dhaila, Bachi Singh oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:371 year:2015 day:12 month:06 pages:244-253 extent:10 https://doi.org/10.1016/j.quaint.2014.10.066 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 371 2015 12 0612 244-253 10 045F 550 |
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10.1016/j.quaint.2014.10.066 doi GBVA2015017000004.pica (DE-627)ELV03472088X (ELSEVIER)S1040-6182(14)00831-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Kotlia, Bahadur Singh verfasserin aut Precipitation variability in the Indian Central Himalaya during last ca. 4,000 years inferred from a speleothem record: Impact of Indian Summer Monsoon (ISM) and Westerlies 2015transfer abstract 10 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. Late Holocene Elsevier Oxygen and carbon isotopes Elsevier Stalagmite Elsevier Westerlies Elsevier Indian Central Himalaya Elsevier Indian Summer Monsoon (ISM) Elsevier Singh, Anoop Kumar oth Joshi, Lalit Mohan oth Dhaila, Bachi Singh oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:371 year:2015 day:12 month:06 pages:244-253 extent:10 https://doi.org/10.1016/j.quaint.2014.10.066 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 371 2015 12 0612 244-253 10 045F 550 |
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10.1016/j.quaint.2014.10.066 doi GBVA2015017000004.pica (DE-627)ELV03472088X (ELSEVIER)S1040-6182(14)00831-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Kotlia, Bahadur Singh verfasserin aut Precipitation variability in the Indian Central Himalaya during last ca. 4,000 years inferred from a speleothem record: Impact of Indian Summer Monsoon (ISM) and Westerlies 2015transfer abstract 10 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. Late Holocene Elsevier Oxygen and carbon isotopes Elsevier Stalagmite Elsevier Westerlies Elsevier Indian Central Himalaya Elsevier Indian Summer Monsoon (ISM) Elsevier Singh, Anoop Kumar oth Joshi, Lalit Mohan oth Dhaila, Bachi Singh oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:371 year:2015 day:12 month:06 pages:244-253 extent:10 https://doi.org/10.1016/j.quaint.2014.10.066 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 371 2015 12 0612 244-253 10 045F 550 |
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10.1016/j.quaint.2014.10.066 doi GBVA2015017000004.pica (DE-627)ELV03472088X (ELSEVIER)S1040-6182(14)00831-3 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Kotlia, Bahadur Singh verfasserin aut Precipitation variability in the Indian Central Himalaya during last ca. 4,000 years inferred from a speleothem record: Impact of Indian Summer Monsoon (ISM) and Westerlies 2015transfer abstract 10 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. Late Holocene Elsevier Oxygen and carbon isotopes Elsevier Stalagmite Elsevier Westerlies Elsevier Indian Central Himalaya Elsevier Indian Summer Monsoon (ISM) Elsevier Singh, Anoop Kumar oth Joshi, Lalit Mohan oth Dhaila, Bachi Singh oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:371 year:2015 day:12 month:06 pages:244-253 extent:10 https://doi.org/10.1016/j.quaint.2014.10.066 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 371 2015 12 0612 244-253 10 045F 550 |
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Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids |
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precipitation variability in the indian central himalaya during last ca. 4,000 years inferred from a speleothem record: impact of indian summer monsoon (ism) and westerlies |
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Precipitation variability in the Indian Central Himalaya during last ca. 4,000 years inferred from a speleothem record: Impact of Indian Summer Monsoon (ISM) and Westerlies |
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We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. |
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We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. |
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We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India. |
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Precipitation variability in the Indian Central Himalaya during last ca. 4,000 years inferred from a speleothem record: Impact of Indian Summer Monsoon (ISM) and Westerlies |
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The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">We report the first high resolution stalagmite record from Indian Central Himalaya by using a combined oxygen and carbon isotopic study spanning the last 4000 years. In addition to the multi-decadal events, the stalagmite data also provide information on the variability in the intensity of precipitation [Indian Summer Monsoon (ISM) and Westerlies] in north Indian hills during the Late Holocene. The δ18O values show strong variability between −2.1‰ and −8.9‰. The extremely high variability points to the monsoon from two different sources compared to other similar aged caves which are primarily controlled by one monsoon, such as the East Asian Summer Monsoon (EASM; although ISM has penetrated into some parts in the areas of EASM in the past) or the Westerlies. Therefore, we suggest that the Westerlies played an important role in the Late Holocene climate of the Indian Himalaya. As the source of the Westerlies is Mediterranean/Atlantic, the North Atlantic Oscillation (NAO) which was responsible for comparatively stronger Westerlies in southern Europe, may have brought higher precipitation to the north Indian hills. The stronger Westerlies may also have resulted in the highest precipitation between 0.5 and 0.25 ka BP (1450–1700 AD; a part of the LIA) in contrast to the weakening of the Indian Summer Monsoon (ISM) in peninsular India. The stalagmite has also recorded the driest period, peaking at ∼3.2 ka BP which may be nearly synchronous with the final collapse of the Harappan culture in northwest India.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Late Holocene</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Oxygen and carbon isotopes</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Stalagmite</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Westerlies</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Indian Central Himalaya</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Indian Summer Monsoon (ISM)</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Singh, Anoop Kumar</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Joshi, Lalit Mohan</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Dhaila, Bachi Singh</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Xiao, Qiuyun ELSEVIER</subfield><subfield code="t">Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids</subfield><subfield code="d">2021</subfield><subfield code="d">the journal of the International Union for Quaternary Research</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV005958261</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:371</subfield><subfield code="g">year:2015</subfield><subfield code="g">day:12</subfield><subfield code="g">month:06</subfield><subfield code="g">pages:244-253</subfield><subfield code="g">extent:10</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.quaint.2014.10.066</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-ASIEN</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">35.00</subfield><subfield code="j">Chemie: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">35.04</subfield><subfield code="j">Ausbildung</subfield><subfield code="j">Beruf</subfield><subfield code="j">Organisationen</subfield><subfield code="x">Chemie</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">371</subfield><subfield code="j">2015</subfield><subfield code="b">12</subfield><subfield code="c">0612</subfield><subfield code="h">244-253</subfield><subfield code="g">10</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">550</subfield></datafield></record></collection>
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