GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 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.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2024-01-30
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉Marine heatwaves are known to have a detrimental impact on marine ecosystems, yet predicting when and where they will occur remains a challenge. Here, using a large ensemble of initialized predictions from an Earth System Model, we demonstrate skill in predictions of summer marine heatwaves over large marine ecosystems in the Arabian Sea seven months ahead. Retrospective forecasts of summer (June to August) marine heatwaves initialized in the preceding winter (November) outperform predictions based on observed frequencies. These predictions benefit from initialization during winters of medium to strong El Niño conditions, which have an impact on marine heatwave characteristics in the Arabian Sea. Our probabilistic predictions target spatial characteristics of marine heatwaves that are specifically useful for fisheries management, as we demonstrate using an example of Indian oil sardine (〈italic〉Sardinella longiceps〈/italic〉).〈/p〉
    Description: Plain Language Summary: Marine heatwaves (MHWs) are prolonged extreme events associated with exceptionally high ocean water temperatures. Such events impose heat stress on marine life, and thus predicting such events is beneficial for management applications. In this work we show that the occurrence of MHWs in summer in the Arabian Sea can be skilfully predicted seven month in advance. Our prediction system benefits from the information of sea surface temperature anomalies in the eastern Pacific Ocean in the preceding winter, among other aspects. Our predictions suggest potential for using climate information in fisheries management in this region.〈/p〉
    Description: Key Points: 〈list list-type="bullet"〉 〈list-item〉 〈p xml:lang="en"〉Summer marine heatwaves in the Arabian Sea are predictable seven months in advance〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉The prediction skill in summer is mainly associated with a preceding El Niño event in winter〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉Probabilistic predictions of Arabian Sea area under heatwave can be tailored to benefit fisheries〈/p〉〈/list-item〉 〈/list〉 〈/p〉
    Description: DFG
    Description: Universität Hamburg http://dx.doi.org/10.13039/501100005711
    Description: Cedars‐Sinai Medical Center http://dx.doi.org/10.13039/100013015
    Description: Marine Institute http://dx.doi.org/10.13039/501100001627
    Description: Copernicus Climate Change Service
    Description: Aigéin, Aeráid, agus athrú Atlantaigh
    Description: EU
    Description: http://dx.doi.org/10.7289/V5SQ8XB5
    Description: http://hdl.handle.net/hdl:21.14106/f2fdc61b13828ed5284f4e4ab41e63f8a84c6e52
    Description: http://hdl.handle.net/hdl:21.14106/27e73ed39cd59d2033e018a494e342383db53a0b
    Keywords: ddc:551.46 ; Arabian Sea ; marine heatwaves
    Language: English
    Type: doc-type:article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2022-05-26
    Description: Author Posting. © The Oceanography Society, 2016. This article is posted here by permission of The Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 29, no. 2 (2016): 38–49, doi:10.5670/oceanog.2016.37.
    Description: The Bay of Bengal (BoB) upper-ocean salinity is examined in the National Centers for Environmental Prediction-Climate Forecasting System version 2 (CFSv2) coupled model, Modular Ocean Model version 5 (MOM5), and Indian National Centre for Ocean Information Services Global Ocean Data Assimilation System (INC-GODAS). CFSv2 displays a large positive salinity bias with respect to World Ocean Atlas 2013 in the upper 40 m of the water column. The prescribed annual mean river discharge and excess evaporation are the main contributors to the positive bias in surface salinity. Overestimation of salinity advection also contributes to the high surface salinity in the model during summer. The surface salinity bias in MOM5 is smaller than in CFSv2 due to prescribed local freshwater flux and seasonally varying river discharge. However, the bias is higher around 70 m in summer and 40 m in fall. This bias is attributed to excessive vertical mixing in the upper ocean. Despite the fact that representation of salinity in INC-GODAS is more realistic due to data assimilation, the vertical mixing scheme still imposes systematic errors. The small-scale processes that control oceanographic turbulence are not adequately resolved in any of these models. Better parameterizations based on dedicated observational programs may help improve freshwater representation in regional and global models.
    Description: TSF acknowledges the support of CSIR, India, for the JRF/SRF Fellowship. HS is grateful for support from the ONR Young Investigator Program (N00014- 15-1-2588).
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 441 (2006), S. 163-165 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Communication between and within cells is essential for the development and survival of any complex organism. Cells converse with each other mainly through a complement of chemical messengers, including neurotransmitters and hormones, that impinge on the cell surface, generating further signals ...
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 364 (1993), S. 814-818 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Xenopus oocytes are widely used as a model system for Ca2 + signalling8'9. Activation of expressed 5-HT receptors that are coupled to InsP3, or injection of non-metabolizable analogues of InsP3, both activate a similar Ca2+ entry pathway through pool depletion7. Thapsigargin, a Ca2+-ATPase ...
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    ISSN: 1432-2013
    Keywords: Calcium current InsP3 Threshold
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract. In many electrically non-excitable cells, Ca2+ entry is mediated predominantly by the store-operated Ca2+ influx pathway. The best-characterised store-operated Ca2+ current is the Ca2+ release-activated Ca2+ current (I CRAC). It is generally believed that high concentrations of intracellular Ca2+ buffer are required to measure I CRAC, due to Ca2+-dependent inactivation of the channels. Recently, we have recorded robust I CRAC in rat basophilic leukaemia (RBL-1) cells at physiological levels of Ca2+ buffering when stores were depleted by inhibition of the sarcoplasmic/ endoplasmic reticulum Ca2+-activated adenosine triphosphatase (SERCA) pumps. However, the second messenger inositol 1,4,5-trisphosphate (InsP3) was not able to evoke the current under such conditions, despite inducing substantial Ca2+ release. We have therefore suggested that a threshold exists within the Ca2+ stores which has to be overcome for macroscopic I CRAC to activate. To establish whether this is a specific feature of I CRAC in RBL-1 cells or whether it is a more general phenomenon, we investigated whether a threshold is also seen in other cell-types used to study store-operated Ca2+ entry. In Jurkat-T lymphocytes, I CRAC is activated weakly by InsP3 in the presence of low concentrations of Ca2+ buffer, whereas the current is large when SERCA pumps are blocked simultaneously, as in RBL-1 cells. Although the electrophysiological properties of I CRAC in the Jurkat cell are very similar to those of RBL-1 cells, the Na+ conductance in the absence of external divalent cations is quite different. Unexpectedly, we failed consistently to record any store-operated Ca2+ current in macrovascular pulmonary artery endothelia whereas robust I CRAC was seen under the same conditions in RBL-1 cells. Our results show that I CRAC has a similar profile of activation in the presence of physiological levels of Ca2+ buffering for Jurkat T-lymphocytes and RBL-1 cells, indicating that the threshold mechanism may be a general feature of I CRAC activation. Because I CRAC in pulmonary artery endothelia is, at best, very small, additional Ca2+ influx pathways may also contribute to agonist-induced Ca2+ entry.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    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
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...