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  • Inositol 1,4,5-triphosphate  (1)
  • Monsoons.  (1)
  • 1
    Online Resource
    Online Resource
    San Diego :Elsevier,
    Keywords: Monsoons. ; Teleconnections (Climatology). ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (496 pages)
    Edition: 1st ed.
    ISBN: 9780128224328
    DDC: 551.5184
    Language: English
    Note: Front cover -- Half title -- Full title -- Copyright -- Contents -- Contributors -- Foreword -- Preface -- Chapter 1 - Drivers of the Indian summer monsoon climate variability -- 1.1 Indian Monsoon as a seasonal phenomena -- 1.2 Synoptic variability and weather systems -- 1.3 Intraseasonal variability -- 1.4 Interannual variability -- 1.5 Decadal variability and climate change -- 1.5.1 Decadal variability -- 1.5.2 Climate change -- 1.6 Summary -- Acknowledgments -- References -- Chapter 2 - Interannual variation of the Indian summer monsoon, ENSO, IOD, and EQUINOO -- 2.1 Introduction -- 2.2 Interaction of atmospheric convection with Pacific and Indian Ocean: ENSO, IOD, and EQUINOO -- 2.3 Monsoon and ENSO -- 2.4 Monsoon and EQUINOO -- 2.5 Monsoon and IOD -- 2.6 Triggering of the favorable phase of EQUINOO/IOD and sustenance of positive EQUINOO during the season -- 2.7 An experiment in prediction of the evolution of EQUINOO and its impact on the monsoon of 2019 -- 2.8 Concluding remarks -- References -- Part I - ENSO-Indian Summer Monsoon teleconnections -- Chapter 3 - ENSO-Indian summer monsoon teleconnections -- 3.1 Introduction -- 3.2 Data -- 3.3 El Niño-Southern Oscillation cycle evolution -- 3.4 ENSO-Indian summer monsoon teleconnections -- 3.4.1 Weakening of ENSO-monsoon relationship -- 3.5 ISMR variability: ENSO and non-ENSO -- 3.6 Summary -- Acknowledgments -- References -- Chapter 4 - ENSO Modoki teleconnections to Indian summer monsoon rainfall-A review -- 4.1 Introduction to ENSO Modoki -- 4.2 Data and methods -- 4.2.1 Criterion for break/active spells -- 4.3 ENSO Modoki and global impacts -- 4.3.1 Characteristics of ENSO Modoki -- 4.3.2 Distinct phenomena, or diversity of ENSOs? -- 4.3.3 Global impacts -- 4.4 Interannual variability of ENSO Modoki-ISM teleconnections. , 4.5 Intraseasonal variability of ENSO Modoki-ISM teleconnections -- References -- Chapter 5 - The decaying phase of El Niño and Indian summer monsoon rainfall -- 5.1 Introduction -- 5.2 Methods and data used -- 5.3 Indian summer monsoon rainfall during El Niño decay -- 5.3.1 Seasonal SST anomalies -- 5.3.2 Monsoonal winds and moisture transport -- 5.4 Summary and discussion -- Acknowledgments -- References -- Chapter 6 - El Niño-Indian summer monsoon relation-a nonlinear scale interactive energy exchange perspective -- 6.1 Introduction -- 6.2 Methodology and formulations -- 6.2.1 Scale selection of El Niño and data -- 6.3 Nonlinear scale interactions between El Niño and Indian summer monsoon -- 6.3.1 El Niño 1997-98 -- 6.3.2 El Niño 2015-16 -- 6.4 Conclusions and discussions -- Acknowledgments -- Appendix -- References -- Chapter 7 - Teleconnections between the Indian summer monsoon and climate variability: a proxy perspective -- 7.1 Introduction -- 7.1.1 Monsoon variability -- 7.1.2 Speleothem -- 7.1.3 Tree rings -- 7.1.4 Marine sediments -- 7.1.5 Proxy's response to forcing mechanism -- 7.1.6 Proxy studies of Indian summer monsoon: scope of the work -- 7.2 Precipitation isotopes: a proxy for large-scale moisture source signature -- 7.3 Proxy evidence of multiple-scale oscillation in Indian summer monsoon -- 7.3.1 Marine records -- 7.3.2 Speleothem records -- 7.3.3 Pacific teleconnections with Indian summer monsoon -- 7.3.4 Atlantic Teleconnections with Indian summer monsoon -- 7.4 Summary and recommendations -- Acknowledgments -- References -- Part II - Indian and Atlantic Ocean - Indian Summer Monsoon teleconnections -- Chapter 8 - Indian Ocean Dipole influence on Indian summer monsoon and ENSO: A review -- 8.1 Introduction -- 8.2 Some salient features of the Indian Ocean Dipole. , 8.3 IOD and the ENSO-monsoon teleconnections: processes at work -- 8.4 Past, present, and future IOD influence on the ENSO-monsoon teleconnection -- 8.5 Challenges and future perspectives -- 8.6 Conclusions -- Conflict of interest statement -- Acknowledgements -- References -- Chapter 9 - Influence of South Tropical Indian Ocean dynamics on the Indian summer monsoon -- 9.1 Introduction -- 9.2 Data and methods -- 9.3 Characteristics of TIO warming and its climatic influence -- 9.3.1 The Southwest Indian Ocean -- 9.3.2 Somalia-Oman upwelling -- 9.3.3 The North Indian Ocean -- 9.3.4 Impacts on Indian summer monsoon -- 9.4 Discussion and summary -- Funding -- Acknowledgements -- References -- Chapter 10 - Atlantic Niño-Indian summer monsoon teleconnections -- 10.1 Introduction -- 10.2 Methods and data -- 10.3 Atlantic Niño and ISM rainfall -- 10.4 Discussion and summary -- Acknowledgement -- References -- Chapter 11 - Teleconnections between tropical SST modes and Indian summer monsoon in observation and CMIP5 models -- 11.1 Introduction -- 11.2 Tropical ocean SST teleconnections to ISM -- 11.2.1 ISM-IOD teleconnection: Observations -- 11.2.2 ISM-IOD teleconnection: model results -- 11.2.3 ISM-ENSO teleconnection -- 11.2.4 ISM in various ENSO phases: historical period -- 11.2.5 ISM in various ENSO phases: historical vs RCP scenario -- 11.3 Mechanisms: role of natural factors -- 11.4 Discussion and summary -- Conflict of Interest -- Funding -- References -- Part III - Subtropical and Extratropical teleconnections to Indian Summer Monsoon -- Chapter 12 - Eurasian snow and the Asian summer monsoon -- 12.1 Introduction -- 12.2 Eurasian snow and the Indian monsoon -- 12.3 Eurasian snow and the East Asian monsoon -- 12.4 Summary and discussion -- Funding -- Acknowledgement -- References. , Chapter 13 - Coupling of the Indian, western North Pacific, and East Asian summer monsoons -- 13.1 Introduction -- 13.2 Data -- 13.3 The tropical pathway -- 13.3.1 The WNP summer monsoon variability -- 13.3.2 Westward influence through atmospheric Rossby waves -- 13.4 The midlatitude pathway -- 13.4.1 The silk road pattern -- 13.4.2 Interaction with the Asian summer monsoons -- 13.5 External drivers of the intermonsoon linkages -- 13.5.1 Concurrent ENSO and the Indian Ocean Dipole mode -- 13.5.2 Decaying ENSO and the IPOC mode -- 13.5.3 External drivers of the silk road pattern -- 13.6 Concluding remarks -- Funding -- References -- Chapter 14 - Teleconnection along the Asian jet stream and its association with the Asian summer monsoon -- 14.1 Introduction -- 14.2 Influences of the SRP/CGT on the ISM and EASM -- 14.3 Influences of the ISM and EASM on the SRP/CGT -- 14.4 Some remaining issues -- 14.5 Summary -- Funding -- References -- Chapter 15 - South Asian summer monsoon and subtropical deserts -- 15.1 Introduction -- 15.2 The monsoon-desert system: background settings -- 15.3 Monsoon influence over hot subtropical deserts -- 15.4 Potential role of deserts in modulating ISM -- 15.5 Summary and future perspectives -- Conflict of interest statement -- Funding -- References -- Chapter 16 - Interaction between South Asian high and Indian Summer Monsoon rainfall -- 16.1   Introduction -- 16.2   Methods and data -- 16.3   Interannual relationship between ISM rainfall and the SAH -- 16.4   Intraseasonal relationship between the ISM rainfall and the SAH zonal shift -- 16.5   Interactive processes on quasi-biweekly time scales -- 16.5.1   Effect of the SAH on the ISM rainfall -- 16.5.2   Effect of the ISM rainfall on the SAH -- 16.6   Summary and Discussion -- Acknowledgment -- References. , Chapter 17 - Southern annular mode teleconnections to Indian summer monsoon -- 17.1 Introduction -- 17.2 Data and methodology -- 17.3 Southern Annular Mode influence on Indian summer monsoon rainfall -- 17.4 Summary and discussion -- Acknowledgments -- References -- Chapter 18 - The Atlantic Multidecadal Oscillation and Indian summer monsoon variability: a revisit -- 18.1 Introduction -- 18.1.1 The Atlantic multidecadal oscillation (AMO) -- 18.2 The statistical AMO-ISM link in the past and present -- 18.3 Mechanisms of the AMO-ISM link -- 18.3.1 Meridional shifts of the ITCZ -- 18.3.2 Direct atmospheric teleconnections -- 18.3.3 Air-sea interactions and Atlantic-Pacific interbasin linkages -- 18.3.4 The role of external forcing -- 18.4 The model-simulated AMO-ISM link -- 18.5 Summary and conclusions -- Acknowledgments -- References -- Chapter 19 - Indian summer monsoon and its teleconnection with Pacific decadal variability -- 19.1 Introduction -- 19.2 Data and methods -- 19.2.1 Data -- 19.2.2 Methods -- 19.3 Pacific decadal variability and Indian summer monsoon -- 19.3.1 Pacific decadal variability -- 19.3.2 Teleconnection of ISMR with IPO -- 19.3.3 Mechanism of IPO-ISMR teleconnection -- 19.3.4 Modeling approach of IPO-ISMR teleconnection -- 19.4 Discussion and summary -- Acknowledgments -- References -- Part IV - Climate change and Monsoon teleconnections -- Chapter 20 - Future changes of the ENSO-Indian summer monsoon teleconnection -- 20.1 Introduction -- 20.2 Data and methods -- 20.2.1 Model data -- 20.2.2 Observations -- 20.2.3 The ensemble-wise method -- 20.3 Past and future changes estimated by the temporal method applied to CMIP6 models -- 20.4 The forced response estimated by the ensemble-wise method for two SMILEs -- 20.5 Summary -- Acknowledgment -- References. , Chapter 21 - Response of the positive Indian Ocean dipole to climate change and impact on Indian summer monsoon rainfall.
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Pflügers Archiv 430 (1995), S. 954-963 
    ISSN: 1432-2013
    Keywords: Ca2+ influx ; Inositol 1,4,5-triphosphate ; Ca2+-activated Cl− current ; Xenopus oocyte
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract The relationship between capacitative Ca2+ influx and activation of Ca2+-dependent Cl− channels was monitored in intactXenopus oocytes following stimulation of 5-hydroxytryptamine (5-HT) receptors, through the activity of Ca2+-dependent Cl− channels using the double-electrode voltage-clamp technique. Under voltage-clamp conditions, 5-HT evoked a rapid transient inward current followed by a slowly developing secondary inward current. The secondary current reflected depletion-activated Ca2+ entry. Hyperpolarising pulses evoked sustained Ca2+-dependent Cl− currents when applied during the transient inward current, but evoked hump-like currents which inactivated rapidly when applied during the secondary inward current. Hump currents arose from Ca2+ entering through the depletion-activated pathway. The hump currents inactivated with hyperpolarising pulses at 〈5-s intervals, and recovered monoexponentially with a time constant of around 8 s. Currents in response to hyperpolarising pulses during the transient current did not inactivate, suggesting that inactivation was associated with Ca2+ entry. When Ca2+ release evoked by inositol 1,4,5-triphosphate [Ins(1,4,5)P 3] was prevented by heparin injection, hyperpolarising pulses during Ca2+ ionophore application also generated hump currents that were dependent on external Ca2+, inactivated and recovered from inactivation with a similar time course as the humps following 5-HT treatment. Pretreatment with the Ca2+ adenosine 5′-triphosphatase (Ca2+ATPase) inhibitor thapsigargin reduced the rate of rise of the hump current, increased the time-to-peak of the current and slowed the rate of decay. Pharmacological interventions to disrupt the cytoskeleton reduced the amplitude of the hump current. It is suggested that, following hyperpolarisation in the presence of Ca2+ entry, the ensuing Ca2+ influx interacts with Cl− channels in a way that might reflect both Ca2+ inhibition of Ca2+ entry and clustering of Cl− channels in the plasma membrane.
    Type of Medium: Electronic Resource
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