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  • 1
    Monograph available for loan
    Monograph available for loan
    Reston, Va. : U.S. Department of the Interior, U.S. Geological Survey
    Call number: M 09.0123
    Type of Medium: Monograph available for loan
    Pages: vi, 75 S.
    ISBN: 9781411322790
    Series Statement: Scientific investigations report / U.S. Geological Survey 2008-5172
    Classification:
    Informatics
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Call number: SR 90.0008(77-13)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 27 S.
    ISBN: 066000836X
    Series Statement: Paper / Geological Survey of Canada 77-13
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 3
    Call number: SR 90.0008(73-25)
    In: Paper
    Type of Medium: Series available for loan
    Pages: 48 S.
    Series Statement: Paper / Geological Survey of Canada 73-25
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
    Series available for loan
    Series available for loan
    Boulder, Colo. : The Geological Society of America
    Associated volumes
    Call number: S 90.0095(397)
    In: Special paper
    Type of Medium: Series available for loan
    Pages: v, 282 S.
    ISBN: 0813723973
    Series Statement: Special paper / Geological Society of America 397
    Classification:
    Informatics
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 5
    Publication Date: 2019-07-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 6
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    Macmillan Publishers Limited
    In:  EPIC3Nature Communications, Macmillan Publishers Limited, 6(6309), pp. 1-8
    Publication Date: 2016-08-30
    Description: Observations show that summer rainfall over large parts of South Asia has declined over the past five to six decades. It remains unclear, however, whether this trend is due to natural variability or increased anthropogenic aerosol loading over South Asia. Here we use stable oxygen isotopes in speleothems from northern India to reconstruct variations in Indian monsoon rainfall over the last two millennia. We find that within the long-term context of our record, the current drying trend is not outside the envelope of monsoon’s oscillatory variability, albeit at the lower edge of this variance. Furthermore, the magnitude of multi-decadal oscillatory variability in monsoon rainfall inferred from our proxy record is comparable to model estimates of anthropogenic-forced trends of mean monsoon rainfall in the 21st century under various emission scenarios. Our results suggest that anthropogenicforced changes in monsoon rainfall will remain difficult to detect against a backdrop of large natural variability
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 7
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    PERGAMON-ELSEVIER SCIENCE LTD
    In:  EPIC3Quaternary Science Reviews, PERGAMON-ELSEVIER SCIENCE LTD, 30, pp. 47-62, ISSN: 0277-3791
    Publication Date: 2019-07-17
    Description: Proxy reconstructions of precipitation from central India, north-central China, and southern Vietnam reveal a series of monsoon droughts during the mid 14th–15th centuries that each lasted for several years to decades. These monsoon megadroughts have no analog during the instrumental period. They occurred in the context of widespread thermal and hydrologic climate anomalies marking the onset of the Little Ice Age (LIA) and appear to have played a major role in shaping significant regional societal changes at that time. New tree ring-width based reconstructions of monsoon variability suggest episodic and widespread reoccurrences of monsoon megadroughts continued throughout the LIA. Although the El-Niño Southern Oscillation (ENSO) plays an important role in monsoon variability, there is no conclusive evidence to suggest that these megadroughts were associated with anomalous sea surface temperature anomalies that were solely the result of ENSO-like variability in the tropical Pacific. Instead, the causative mechanisms of these megadroughts may reside in protracted changes in the synoptic-scale monsoon climatology of the Indian Ocean. Today, the intra-seasonal monsoon variability is dominated by ‘active’ and the ‘break’ spells – two distinct oscillatory modes of monsoon that have radically different synoptic scale circulation and precipitation patterns. We suggest that protracted locking of the monsoon into the “break-dominated” mode – a mode that favors reduced precipitation over the Indian sub-continent and SE Asia and enhanced precipitation over the equatorial Indian Ocean, may have caused these exceptional droughts. Impetus for periodic locking of the monsoon into this mode may have been provided by cooler temperatures at the extratropical latitudes in the Northern Hemisphere which forced the mean position of the Inter-Tropical Convergence Zone (ITCZ) further southward in the Indian Ocean.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 8
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    AMER GEOPHYSICAL UNION
    In:  EPIC3Geophysical Research Letters, AMER GEOPHYSICAL UNION, 38, pp. L15703, ISSN: 0094-8276
    Publication Date: 2019-07-17
    Description: The “internally” generated intraseasonal variability of the Indian Summer Monsoon is characterized by intermittent periods of enhanced (“active”) and deficient (“break”) precipitation, which produce a quasi east-west precipitation dipole over the Indian subcontinent. Here we present multicentennial-length and near annually-resolved reconstructions of monsoon precipitation, inferred from absolute-dated and instrumentally calibrated speleothem oxygen isotope records from regions (central and northeast India) that have diametric responses to active-break monsoon circulation patterns. On centennial timescales (AD 1400–2008), precipitation variability from these two regions exhibit opposing behavior, oscillating between periods with a persistently “active-dominated” (AD ∼1700 to 2007) and a “break-dominated” (AD 1400 to ∼1700) regime. The switch between these regimes occurs abruptly (within decades) at a time (AD ∼ 1650–1700) when a proxy record of upwelling intensity from the Arabian Sea suggest an abrupt increase in the monsoon winds. On the basis of these observations, we hypothesize that the frequency distribution of active-break periods varies on centennial timescales, implying a leading role of internal dynamics in governing the ISM response to slowly-evolving changes in the external boundary conditions.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 9
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    Copernicus
    In:  EPIC3Climate of the Past Discussions, Copernicus, 9, pp. 3103-3123, ISSN: 1814-9324
    Publication Date: 2019-07-17
    Description: There are a number of clear examples in the instrumental period where positive El Niño events were coincident with a severely weakened summer monsoon over India (ISM). ENSO's influence on the Indian Monsoon has therefore remained the centerpiece of various predictive schemes of ISM rainfall for over a century. The teleconnection between the monsoon and ENSO has undergone a protracted weakening since the late 1980's suggesting the strength of ENSO's influence on the monsoon may vary considerably on multidecadal timescales. The recent weakening has specifically prompted questions as to whether this shift represents a natural mode of climate variability or a fundamental change in ENSO and/or ISM dynamics due to anthropogenic warming. The brevity of empirical observations and large systematic errors in the representation of these two systems in state-of-the-art general circulation models hamper efforts to reliably assess the low frequency nature of this dynamical coupling under varying climate forcings. Here we place the 20th century ENSO-Monsoon relationship in a millennial context by assessing the phase angle between the two systems across the time spectrum using a continuous tree-ring ENSO reconstruction from North America and a speleothem oxygen isotope (δ18O) based reconstruction of the ISM. The results suggest that in the high-frequency domain (≤ 15 yr), El Niño (La Niña) events persistently lead to a weakened (strengthened) monsoon consistent with the observed relationship between the two systems during the instrumental period. However, in the low frequency domain (≥ 60 yr), periods of strong monsoon are, in general, coincident with periods of enhanced ENSO variance. This relationship is opposite to which would be predicted dynamically and leads us to conclude that ENSO is not pacing the prominent multidecadal variability that has characterized the ISM over the last millennium.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , notRev
    Format: application/pdf
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  • 10
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    In:  http://aquaticcommons.org/id/eprint/16506 | 12051 | 2015-04-03 06:43:03 | 16506 | Indian Fisheries Association
    Publication Date: 2021-07-06
    Description: A feeding trial was conducted to study the role of vitamin E in growth of Catla catla fry. Newly hatched larvae of Catla were fed with synthetic diet, supplemented with graded levels of vitamin E α0, 50, 100, 150, 200, 250 mg/Kg of diet. The spawn were fed with five times of their body weight for 30 days. Observation was made on the basis of survival, growth, daily weight gain and food conversion ratio. The significant weight gain and highest survival could be achieved by the diet supplemented with 150 mg of vitamin E per kg of the diet. The weight gain per day in 0, 50, 100, 150, 200 and 250 mg vitamin F/kg supplemented diet were 4.0, 5.2, 6.5, 7.8, 6.8 and 6.3 mg, while survival was 50, 51.8, 52.4, 52.8, 52.2 and 52% respectively.
    Description: Paper presented at the National Symposium on Aquacrops, 16-18 November 1994, Versova, Bombay (India)
    Keywords: Aquaculture ; nutritional requirements ; freshwater fish ; food conversion ; Catla catla ; feeding trials
    Repository Name: AquaDocs
    Type: article
    Format: application/pdf
    Format: application/pdf
    Format: 91-96
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