GLORIA

GEOMAR Library Ocean Research Information Access

X

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
    What causes southeast Australia's worst droughts?
    American Geophysical Union (AGU) ; 2009
    In:  Geophysical Research Letters Vol. 36, No. 4 ( 2009-02-24)
    Details
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 36, No. 4 ( 2009-02-24)
    Type of Medium: Online Resource
    ISSN: 0094-8276
    URL: Article
    DOI: 10.1029/2008GL036801
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2009
    detail.hit.zdb_id: 2021599-X
    detail.hit.zdb_id: 7403-2
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    Online Resource
  • 2
    Online Resource
    Online Resource
    On the Dynamics of Austral Heat Waves
    American Geophysical Union (AGU) ; 2018
    In:  Journal of Geophysical Research: Atmospheres Vol. 123, No. 1 ( 2018-01-16), p. 38-57
    Details
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 123, No. 1 ( 2018-01-16), p. 38-57
    Abstract: Australian heat waves occur in conjunction with activated blocking nodes of planetary waveguide modes Heat waves are preceded by upstream expression and followed by downstream expression of the planetary waveguide modes The heat wave blocking high is maintained by convergence of wave activity in a well‐defined wave channel
    Type of Medium: Online Resource
    ISSN: 2169-897X , 2169-8996
    URL: Issue
    URL: Article
    DOI: 10.1002/jgrd.v123.1
    DOI: 10.1002/2017JD027222
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2018
    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 2969341-X
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    Online Resource
  • 3
    Online Resource
    Online Resource
    Internal climate memory in observations and models
    American Geophysical Union (AGU) ; 2015
    In:  Geophysical Research Letters Vol. 42, No. 4 ( 2015-02-28), p. 1232-1242
    Details
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 42, No. 4 ( 2015-02-28), p. 1232-1242
    Abstract: Beyond 5 years little variance evident in the tropics Southern Hemisphere oceans variance maxima are in subtropical baroclinic zones Memory on longer time scales is related to identifiable dynamical processes
    Type of Medium: Online Resource
    ISSN: 0094-8276 , 1944-8007
    URL: Issue
    URL: Article
    DOI: 10.1002/grl.v42.4
    DOI: 10.1002/2014GL062765
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2015
    detail.hit.zdb_id: 2021599-X
    detail.hit.zdb_id: 7403-2
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    Online Resource
  • 4
    Online Resource
    Online Resource
    A multiproxy index of the El Niño–Southern Oscillation, A.D. 1525–1982
    American Geophysical Union (AGU) ; 2009
    In:  Journal of Geophysical Research Vol. 114, No. D5 ( 2009-03-06)
    Details
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 114, No. D5 ( 2009-03-06)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    URL: Article
    DOI: 10.1029/2008JD010896
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2009
    detail.hit.zdb_id: 2033040-6
    detail.hit.zdb_id: 3094104-0
    detail.hit.zdb_id: 2130824-X
    detail.hit.zdb_id: 2016813-5
    detail.hit.zdb_id: 2016810-X
    detail.hit.zdb_id: 2403298-0
    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 161666-3
    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
    detail.hit.zdb_id: 3094268-8
    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    Online Resource
  • 5
    Online Resource
    Online Resource
    Sensitivity of a meridional temperature gradient index to latitudinal domain
    American Geophysical Union (AGU) ; 1999
    In:  Journal of Geophysical Research: Atmospheres Vol. 104, No. D14 ( 1999-07-27), p. 16709-16717
    Details
    In: Journal of Geophysical Research: Atmospheres, American Geophysical Union (AGU), Vol. 104, No. D14 ( 1999-07-27), p. 16709-16717
    Abstract: We compare two alternative definitions of the meridional surface temperature gradient (MTG) in the northern hemisphere. One focuses on equator‐pole differences ((0°–25°N)–(65°–90°N)) and the other focuses on differences over midlatitudes ((30°–35°N)–(50°–55°N)). The MTG is sensitive to the choice of latitudes used to define it, and these two MTGs show substantial differences in behavior on timescales from interannual to multidecadal. The equator‐pole MTG is plagued by missing data in the high‐latitude belt, which affects its characteristics over at least the early part of the data record. Because the missing data are concentrated most heavily in the northernmost zones of the high‐latitude belt, the variance of the equator‐pole MTG is unduly high. This suggests a need to weight the equator‐pole MTG by data availability in each latitude zone. The midlatitude‐oriented MTG is more robust with respect to data availability and provides a measure of midlatitude circulation features.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    URL: Article
    DOI: 10.1029/1999JD900223
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1999
    detail.hit.zdb_id: 2033040-6
    detail.hit.zdb_id: 3094104-0
    detail.hit.zdb_id: 2130824-X
    detail.hit.zdb_id: 2016813-5
    detail.hit.zdb_id: 2016810-X
    detail.hit.zdb_id: 2403298-0
    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 161666-3
    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
    detail.hit.zdb_id: 3094268-8
    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    Online Resource
  • 6
    Online Resource
    Online Resource
    Do we know what difference a delay makes?
    American Geophysical Union (AGU) ; 1991
    In:  Eos, Transactions American Geophysical Union Vol. 72, No. 53 ( 1991-12-31), p. 593-593
    Details
    In: Eos, Transactions American Geophysical Union, American Geophysical Union (AGU), Vol. 72, No. 53 ( 1991-12-31), p. 593-593
    Abstract: In our original comment [ Risbey et al. ., 1991] we argued that the work of Schlesinger and Jiang [1991a] is too limited to determine whether or not (as they put it) “the penalty is small for a 10‐year delay in initiating the transition to a regime in which greenhouse‐gas emissions are reduced.” In their reply, Schlesinger and Jiang [1991b] (hereafter S & J) presented their reasons for concluding definitively that the penalty is small. However S & J's discussion of the evidence and literature on climate change and greenhouse warming contains significant omissions and mis‐statements. In dismissing our concern that their model was too simple to evaluate the possibility of abrupt climate change, S & J rely on results from coupled ocean‐atmosphere general circulation models (GCMs), in particular the work of Cubasch et al. . [1991]. Here S & J make two claims, one of which is incorrect and the other questionable. First, they claim that “the coupled atmosphere‐ocean model of Cubasch et al. [1991] does allow the nonlinearities that Risbey et al. . [1991] criticize our simple model for not including.” In fact we explicitly mentioned changes in polar ice caps [ Oerlemans and van der Veen , 1984] and release of methane from clathrates [ MacDonald , 1990; Bell , 1982], neither of which are included in the model of Cubasch et al. . [1991]. Indeed, none of the published simulations of global warming using coupled ocean‐atmosphere GCMs include these effects. Nor do these models yet include in their enhanced greenhouse simulations many of the possible feedbacks involving the carbon cycle and biosphere [ Lashof , 1989; Bacastow and Maier‐Reimer , 1990; Sellers , 1987] that could significantly alter greenhouse gas concentrations and surface properties. The published simulations with these models do allow for some changes in deep ocean circulation and cloud behavior, but there is controversy over whether they correctly represent these processes [ Marotzke , 1991; Mitchell , 1989; Cess , 1990]. In addition the coupled models must be arbitrarily tuned (requiring substantial artificial fluxes of heat and moisture) to get the current climate right [ Manabe et al. ., 1991; Cubasch et al. ., 1991]. Their greenhouse change simulations are at least partly constrained by these flux adjustments.
    Type of Medium: Online Resource
    ISSN: 0096-3941 , 2324-9250
    URL: Article
    DOI: 10.1029/90EO00413
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1991
    detail.hit.zdb_id: 24845-9
    detail.hit.zdb_id: 2118760-5
    detail.hit.zdb_id: 240154-X
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    Online Resource
  • 7
    Online Resource
    Online Resource
    Spatial trends in synoptic rainfall in southern Australia
    American Geophysical Union (AGU) ; 2013
    In:  Geophysical Research Letters Vol. 40, No. 14 ( 2013-07-28), p. 3781-3785
    Details
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 40, No. 14 ( 2013-07-28), p. 3781-3785
    Abstract: Rainfall variations can be assessed by synoptic typing The key types for southern Australia are cold fronts and cutoff lows Longitudinal variations are important for assessing trends
    Type of Medium: Online Resource
    ISSN: 0094-8276 , 1944-8007
    URL: Issue
    URL: Article
    DOI: 10.1002/grl.v40.14
    DOI: 10.1002/grl.50739
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2013
    detail.hit.zdb_id: 2021599-X
    detail.hit.zdb_id: 7403-2
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    Online Resource
  • 8
    Online Resource
    Online Resource
    The greenhouse debate: Time for action?
    American Geophysical Union (AGU) ; 1991
    In:  Eos, Transactions American Geophysical Union Vol. 72, No. 53 ( 1991-12-31), p. 593-600
    Details
    In: Eos, Transactions American Geophysical Union, American Geophysical Union (AGU), Vol. 72, No. 53 ( 1991-12-31), p. 593-600
    Abstract: In recent years, debate has intensified over whether to act now or delay actions that would reduce emissions of greenhouse gases. In a recent contribution to this debate in Nature, Schlesinger and Jiang [1991] conclude that “the penalty is small for a 10‐year delay in initiating the transition to a regime in which greenhouse‐gas emissions are reduced.” This conclusion is premature, since these authors did not consider a number of pertinent factors. Schlesinger and Jiang used a simple energy‐ balance climate model with an upwelling‐ diffusion ocean to examine the surface temperature response to transitions between various Intergovernmental Panel on Climate Change (IPCC) [ Houghton et al ., 1990] trace gas scenarios. They found that “a delay of 10 years in initiating a 20‐year transition from the IPCC [business as usual] scenario to any other IPCC scenario has only a small effect on the projected warming in 2100.” From this they concluded that “the penalty for a 10‐year delay is small.” We offer several reasons why we think this is a non sequitur.
    Type of Medium: Online Resource
    ISSN: 0096-3941 , 2324-9250
    URL: Article
    DOI: 10.1029/90EO10412
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1991
    detail.hit.zdb_id: 24845-9
    detail.hit.zdb_id: 2118760-5
    detail.hit.zdb_id: 240154-X
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    Online Resource
  • 9
    Online Resource
    Online Resource
    On the limitations of general circulation climate models
    American Geophysical Union (AGU) ; 1990
    In:  Geophysical Research Letters Vol. 17, No. 12 ( 1990-11), p. 2173-2176
    Details
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 17, No. 12 ( 1990-11), p. 2173-2176
    Type of Medium: Online Resource
    ISSN: 0094-8276
    URL: Article
    DOI: 10.1029/GL017i012p02173
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1990
    detail.hit.zdb_id: 2021599-X
    detail.hit.zdb_id: 7403-2
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    Online Resource
  • 10
    Online Resource
    Online Resource
    Trends in the surface meridional temperature gradient
    American Geophysical Union (AGU) ; 1997
    In:  Geophysical Research Letters Vol. 24, No. 10 ( 1997-05-15), p. 1243-1246
    Details
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 24, No. 10 ( 1997-05-15), p. 1243-1246
    Abstract: Given the presence of a meridional temperature gradient (MTG) across midlatitudes, large‐scale eddies transport heat poleward, thereby shaping Earth's climate. Defining an MTG index here as the difference in surface temperature between the 30°–35°N belt and the 50°–55°N belt, we use a temperature record compiled from observations over a 110‐year period to determine a trend in the MTG in the last century. We find a significant decreasing trend in the MTG over this period of 0.4±0.1°C per 100 years, along with indications of substantial multidecadal variability.
    Type of Medium: Online Resource
    ISSN: 0094-8276 , 1944-8007
    URL: Article
    DOI: 10.1029/97GL01154
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1997
    detail.hit.zdb_id: 2021599-X
    detail.hit.zdb_id: 7403-2
    SSG: 16,13
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
    Online Resource
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...