Ram R Yadav
Biographic Data
| ID | 4785279 |
|---|---|
| NAME | Ram R Yadav |
| GIVEN NAMES | Ram R |
| FAMILY NAME | Yadav |
| SIGNATURE | YADAV R R |
| AFFILIATIONS | Birbal Sahni Institute of Palaeosciences |
| ORCID | 0000-0003-1068-7195 |
| VERIFIED | Yes |
| TOTAL WORKS | 16 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 16 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1992 |
| LATEST PUBLICATION YEAR | 2023 |
| H-INDEX | 0 |
Temperature variability over Dokriani glacier region, Western Himalaya, India
Sub-alpine trees testify late 20th century rapid retreat of Gangotri glacier, Central Himalaya
Tree-ring δ18O records of abating June–July monsoon rainfall over the Himalayan region in the last 273 years
Altitudinal treeline dynamics of Himalayan pine in western Himalaya, India
Tree ring drought records from Kishtwar, Jammu and Kashmir, northwest Himalaya, India
Tree ring evidence of late summer warming in Sikkim, northeast India
Satluj river flow variations since AD 1660 based on tree-ring network of Himalayan cedar from western Himalaya, India
Premonsoon precipitation variability in Kumaon Himalaya, India over a perspective of ∼300 years
February–June temperature variability in western Himalaya, India, since AD 1455
Tree-ring-based seven century long flow records of Satluj River, western Himalaya, India
Relationship between winter precipitation over the western Himalaya and central northeast India summer monsoon rainfall
Tree-Ring-Based Spring Temperature Patterns over the Past Four Centuries in Western Himalaya
A network of 12 tree-ring width chronologies of Himalayan cedar ( Cedrus deodara ) from the western Himalayan region, India, has been used to reconstruct mean spring (March–May) temperature variations back to A.D. 1600. The most conspicuous feature of the temperature reconstruction is the long-term cooling trend since the late 17th century that ended early in the 20th century. The warmest 30-yr mean for the 20th century was recorded during 1945–1…
Spring-temperature variations in western Himalaya, India, as reconstructed from tree-rings
The Himalayan region plays a very important role in influencing the regional and extra-regional circulation system. Long-term instrumental or proxy climate records for this region are scant, but are essential for a global perspective of climate variability. A 598-year (AD 1390-1987) reconstruction of spring (March-May) temperature has been derived for the first time for the western Himalayan region, India using a well replicated ring-width chrono…
Dendroclimatic Reconstruction of April–May Temperature Fluctuations in the Western Himalaya of India Since A.D. 1698
Ring-width chronologies of Himalayan cedar ( Cedrus deodara (D. Don.) G. Don.), Himalayan pine ( Pinus wallichiana A. B. Jackson), and Himalayan spruce ( Picea smithiana (Wall.) Boiss.) from the western Himalayan region, India, have been used to reconstruct mean April–May temperature back to A. D. 1698. The reconstruction correlates significantly with the average April–May instrumental temperature record ( r = +0.62, 1876–1988) and is characteriz…
Dendroindications of recent volcanic eruptions in Kamchatka, Russia
Precisely dated tree-ring sequences of larch (Larix cajanderi Mayr) extending from 1801–1980 ad from Kamchatka lying in the far east of Asian continent were studied to see the influence of volcanic eruptions on tree growth and to assess the potential of tree rings for dating ancient volcanic events. Nearby volcanic events are clearly reflected in ring-width patterns. Distinctly narrow rings are formed in the year following the year of eruption. W…
Dating of Earthquakes
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Dendroindications of recent volcanic eruptions in Kamchatka, Russia
Precisely dated tree-ring sequences of larch (Larix cajanderi Mayr) extending from 1801–1980 ad from Kamchatka lying in the far east of Asian continent were studied to see the influence of volcanic eruptions on tree growth and to assess the potential of tree rings for dating ancient volcanic events. Nearby volcanic events are clearly reflected in ring-width patterns. Distinctly narrow rings are formed in the year following the year of eruption. W…
Dating of Earthquakes
Dendroclimatic Reconstruction of April–May Temperature Fluctuations in the Western Himalaya of India Since A.D. 1698
Ring-width chronologies of Himalayan cedar ( Cedrus deodara (D. Don.) G. Don.), Himalayan pine ( Pinus wallichiana A. B. Jackson), and Himalayan spruce ( Picea smithiana (Wall.) Boiss.) from the western Himalayan region, India, have been used to reconstruct mean April–May temperature back to A. D. 1698. The reconstruction correlates significantly with the average April–May instrumental temperature record ( r = +0.62, 1876–1988) and is characteriz…
Spring-temperature variations in western Himalaya, India, as reconstructed from tree-rings
The Himalayan region plays a very important role in influencing the regional and extra-regional circulation system. Long-term instrumental or proxy climate records for this region are scant, but are essential for a global perspective of climate variability. A 598-year (AD 1390-1987) reconstruction of spring (March-May) temperature has been derived for the first time for the western Himalayan region, India using a well replicated ring-width chrono…
Tree-Ring-Based Spring Temperature Patterns over the Past Four Centuries in Western Himalaya
A network of 12 tree-ring width chronologies of Himalayan cedar ( Cedrus deodara ) from the western Himalayan region, India, has been used to reconstruct mean spring (March–May) temperature variations back to A.D. 1600. The most conspicuous feature of the temperature reconstruction is the long-term cooling trend since the late 17th century that ended early in the 20th century. The warmest 30-yr mean for the 20th century was recorded during 1945–1…
Tree-ring-based seven century long flow records of Satluj River, western Himalaya, India
Relationship between winter precipitation over the western Himalaya and central northeast India summer monsoon rainfall
Premonsoon precipitation variability in Kumaon Himalaya, India over a perspective of ∼300 years
February–June temperature variability in western Himalaya, India, since AD 1455
Tree ring evidence of late summer warming in Sikkim, northeast India
Satluj river flow variations since AD 1660 based on tree-ring network of Himalayan cedar from western Himalaya, India
Altitudinal treeline dynamics of Himalayan pine in western Himalaya, India
Tree ring drought records from Kishtwar, Jammu and Kashmir, northwest Himalaya, India
Tree-ring δ18O records of abating June–July monsoon rainfall over the Himalayan region in the last 273 years
Sub-alpine trees testify late 20th century rapid retreat of Gangotri glacier, Central Himalaya
Temperature variability over Dokriani glacier region, Western Himalaya, India
Geography (15 works) · Tree-ring climate responses (15 works) · Physical geography (14 works) · Climatology (13 works) · Geology (13 works) · Dendrochronology (11 works) · Plant Water Relations and Carbon Dynamics (11 works) · Climate change (7 works) · Chronology (6 works) · Geology and Paleoclimatology Research (6 works)