The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model
Summary The factors that control the strength of the ITCZ (Inter Tropical Convergence Zone) in an aquaplanet GCM (General Circulation Model) have been investigated. The strength of the equatorial ITCZ was found to increase rapidly with increase in meridional gradient of SST. On the other hand, the s...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Vidyunmala, V. [verfasserIn] Nanjundiah, R. S. [verfasserIn] Srinivasan, J. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2006 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Meteorology and atmospheric physics - Wien [u.a.] : Springer, 1948, 95(2006), 3-4 vom: 12. Sept., Seite 239-253 |
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| Übergeordnetes Werk: |
volume:95 ; year:2006 ; number:3-4 ; day:12 ; month:09 ; pages:239-253 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00703-006-0206-7 |
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| Katalog-ID: |
SPR007306695 |
|---|
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| 100 | 1 | |a Vidyunmala, V. |e verfasserin |4 aut | |
| 245 | 1 | 4 | |a The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model |
| 264 | 1 | |c 2006 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a Computermedien |b c |2 rdamedia | ||
| 338 | |a Online-Ressource |b cr |2 rdacarrier | ||
| 520 | |a Summary The factors that control the strength of the ITCZ (Inter Tropical Convergence Zone) in an aquaplanet GCM (General Circulation Model) have been investigated. The strength of the equatorial ITCZ was found to increase rapidly with increase in meridional gradient of SST. On the other hand, the strength of the off-equatorial ITCZ does not increase rapidly with increase in meridional gradient of SST. This unusual difference in behavior between off-equatorial and equatorial ITCZ has been interpreted with a diagnostic model. The diagnostic model is based on budgets of moisture and dry static energy in the ITCZ. The diagnostic model indicates that the variations in the strength of the ITCZ are related to changes in the net energy convergence and vertical moist static stability. It was found that the net energy convergence in the off-equatorial ITCZ increases much less rapidly with meridional SST gradient than the equatorial counterpart. This difference in the behavior of net energy convergence is related to the surface wind speed which in the off-equatorial ITCZ simulation is largely insensitive to changes in the meridional SST gradient. Thus the primary difference between the equatorial and off-equatorial ITCZ is on account of the fact that wind speeds were lower in the former (on account of the constraint that zonal wind has to be zero at the equator). The impact of increasing the SST maximum on the strength of the ITCZ has also been studied. It was found that the strength of ITCZ increases with an increase in SST maximum. This increase in the strength of the ITCZ with the maximum SST is governed by the increase in boundary layer specific humidity and its impact on vertical moist static stability. | ||
| 650 | 4 | |a Surface Wind Speed |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Hadley Circulation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Moisture Convergence |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Diagnostic Model |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Meridional Gradient |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Nanjundiah, R. S. |e verfasserin |4 aut | |
| 700 | 1 | |a Srinivasan, J. |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Meteorology and atmospheric physics |d Wien [u.a.] : Springer, 1948 |g 95(2006), 3-4 vom: 12. Sept., Seite 239-253 |w (DE-627)25463091X |w (DE-600)1462145-9 |x 1436-5065 |7 nnns |
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10.1007/s00703-006-0206-7 doi (DE-627)SPR007306695 (SPR)s00703-006-0206-7-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Vidyunmala, V. verfasserin aut The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary The factors that control the strength of the ITCZ (Inter Tropical Convergence Zone) in an aquaplanet GCM (General Circulation Model) have been investigated. The strength of the equatorial ITCZ was found to increase rapidly with increase in meridional gradient of SST. On the other hand, the strength of the off-equatorial ITCZ does not increase rapidly with increase in meridional gradient of SST. This unusual difference in behavior between off-equatorial and equatorial ITCZ has been interpreted with a diagnostic model. The diagnostic model is based on budgets of moisture and dry static energy in the ITCZ. The diagnostic model indicates that the variations in the strength of the ITCZ are related to changes in the net energy convergence and vertical moist static stability. It was found that the net energy convergence in the off-equatorial ITCZ increases much less rapidly with meridional SST gradient than the equatorial counterpart. This difference in the behavior of net energy convergence is related to the surface wind speed which in the off-equatorial ITCZ simulation is largely insensitive to changes in the meridional SST gradient. Thus the primary difference between the equatorial and off-equatorial ITCZ is on account of the fact that wind speeds were lower in the former (on account of the constraint that zonal wind has to be zero at the equator). The impact of increasing the SST maximum on the strength of the ITCZ has also been studied. It was found that the strength of ITCZ increases with an increase in SST maximum. This increase in the strength of the ITCZ with the maximum SST is governed by the increase in boundary layer specific humidity and its impact on vertical moist static stability. Surface Wind Speed (dpeaa)DE-He213 Hadley Circulation (dpeaa)DE-He213 Moisture Convergence (dpeaa)DE-He213 Diagnostic Model (dpeaa)DE-He213 Meridional Gradient (dpeaa)DE-He213 Nanjundiah, R. S. verfasserin aut Srinivasan, J. verfasserin aut Enthalten in Meteorology and atmospheric physics Wien [u.a.] : Springer, 1948 95(2006), 3-4 vom: 12. Sept., Seite 239-253 (DE-627)25463091X (DE-600)1462145-9 1436-5065 nnns volume:95 year:2006 number:3-4 day:12 month:09 pages:239-253 https://dx.doi.org/10.1007/s00703-006-0206-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE AR 95 2006 3-4 12 09 239-253 |
| spelling |
10.1007/s00703-006-0206-7 doi (DE-627)SPR007306695 (SPR)s00703-006-0206-7-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Vidyunmala, V. verfasserin aut The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary The factors that control the strength of the ITCZ (Inter Tropical Convergence Zone) in an aquaplanet GCM (General Circulation Model) have been investigated. The strength of the equatorial ITCZ was found to increase rapidly with increase in meridional gradient of SST. On the other hand, the strength of the off-equatorial ITCZ does not increase rapidly with increase in meridional gradient of SST. This unusual difference in behavior between off-equatorial and equatorial ITCZ has been interpreted with a diagnostic model. The diagnostic model is based on budgets of moisture and dry static energy in the ITCZ. The diagnostic model indicates that the variations in the strength of the ITCZ are related to changes in the net energy convergence and vertical moist static stability. It was found that the net energy convergence in the off-equatorial ITCZ increases much less rapidly with meridional SST gradient than the equatorial counterpart. This difference in the behavior of net energy convergence is related to the surface wind speed which in the off-equatorial ITCZ simulation is largely insensitive to changes in the meridional SST gradient. Thus the primary difference between the equatorial and off-equatorial ITCZ is on account of the fact that wind speeds were lower in the former (on account of the constraint that zonal wind has to be zero at the equator). The impact of increasing the SST maximum on the strength of the ITCZ has also been studied. It was found that the strength of ITCZ increases with an increase in SST maximum. This increase in the strength of the ITCZ with the maximum SST is governed by the increase in boundary layer specific humidity and its impact on vertical moist static stability. Surface Wind Speed (dpeaa)DE-He213 Hadley Circulation (dpeaa)DE-He213 Moisture Convergence (dpeaa)DE-He213 Diagnostic Model (dpeaa)DE-He213 Meridional Gradient (dpeaa)DE-He213 Nanjundiah, R. S. verfasserin aut Srinivasan, J. verfasserin aut Enthalten in Meteorology and atmospheric physics Wien [u.a.] : Springer, 1948 95(2006), 3-4 vom: 12. Sept., Seite 239-253 (DE-627)25463091X (DE-600)1462145-9 1436-5065 nnns volume:95 year:2006 number:3-4 day:12 month:09 pages:239-253 https://dx.doi.org/10.1007/s00703-006-0206-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE AR 95 2006 3-4 12 09 239-253 |
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10.1007/s00703-006-0206-7 doi (DE-627)SPR007306695 (SPR)s00703-006-0206-7-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Vidyunmala, V. verfasserin aut The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary The factors that control the strength of the ITCZ (Inter Tropical Convergence Zone) in an aquaplanet GCM (General Circulation Model) have been investigated. The strength of the equatorial ITCZ was found to increase rapidly with increase in meridional gradient of SST. On the other hand, the strength of the off-equatorial ITCZ does not increase rapidly with increase in meridional gradient of SST. This unusual difference in behavior between off-equatorial and equatorial ITCZ has been interpreted with a diagnostic model. The diagnostic model is based on budgets of moisture and dry static energy in the ITCZ. The diagnostic model indicates that the variations in the strength of the ITCZ are related to changes in the net energy convergence and vertical moist static stability. It was found that the net energy convergence in the off-equatorial ITCZ increases much less rapidly with meridional SST gradient than the equatorial counterpart. This difference in the behavior of net energy convergence is related to the surface wind speed which in the off-equatorial ITCZ simulation is largely insensitive to changes in the meridional SST gradient. Thus the primary difference between the equatorial and off-equatorial ITCZ is on account of the fact that wind speeds were lower in the former (on account of the constraint that zonal wind has to be zero at the equator). The impact of increasing the SST maximum on the strength of the ITCZ has also been studied. It was found that the strength of ITCZ increases with an increase in SST maximum. This increase in the strength of the ITCZ with the maximum SST is governed by the increase in boundary layer specific humidity and its impact on vertical moist static stability. Surface Wind Speed (dpeaa)DE-He213 Hadley Circulation (dpeaa)DE-He213 Moisture Convergence (dpeaa)DE-He213 Diagnostic Model (dpeaa)DE-He213 Meridional Gradient (dpeaa)DE-He213 Nanjundiah, R. S. verfasserin aut Srinivasan, J. verfasserin aut Enthalten in Meteorology and atmospheric physics Wien [u.a.] : Springer, 1948 95(2006), 3-4 vom: 12. Sept., Seite 239-253 (DE-627)25463091X (DE-600)1462145-9 1436-5065 nnns volume:95 year:2006 number:3-4 day:12 month:09 pages:239-253 https://dx.doi.org/10.1007/s00703-006-0206-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE AR 95 2006 3-4 12 09 239-253 |
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10.1007/s00703-006-0206-7 doi (DE-627)SPR007306695 (SPR)s00703-006-0206-7-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Vidyunmala, V. verfasserin aut The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary The factors that control the strength of the ITCZ (Inter Tropical Convergence Zone) in an aquaplanet GCM (General Circulation Model) have been investigated. The strength of the equatorial ITCZ was found to increase rapidly with increase in meridional gradient of SST. On the other hand, the strength of the off-equatorial ITCZ does not increase rapidly with increase in meridional gradient of SST. This unusual difference in behavior between off-equatorial and equatorial ITCZ has been interpreted with a diagnostic model. The diagnostic model is based on budgets of moisture and dry static energy in the ITCZ. The diagnostic model indicates that the variations in the strength of the ITCZ are related to changes in the net energy convergence and vertical moist static stability. It was found that the net energy convergence in the off-equatorial ITCZ increases much less rapidly with meridional SST gradient than the equatorial counterpart. This difference in the behavior of net energy convergence is related to the surface wind speed which in the off-equatorial ITCZ simulation is largely insensitive to changes in the meridional SST gradient. Thus the primary difference between the equatorial and off-equatorial ITCZ is on account of the fact that wind speeds were lower in the former (on account of the constraint that zonal wind has to be zero at the equator). The impact of increasing the SST maximum on the strength of the ITCZ has also been studied. It was found that the strength of ITCZ increases with an increase in SST maximum. This increase in the strength of the ITCZ with the maximum SST is governed by the increase in boundary layer specific humidity and its impact on vertical moist static stability. Surface Wind Speed (dpeaa)DE-He213 Hadley Circulation (dpeaa)DE-He213 Moisture Convergence (dpeaa)DE-He213 Diagnostic Model (dpeaa)DE-He213 Meridional Gradient (dpeaa)DE-He213 Nanjundiah, R. S. verfasserin aut Srinivasan, J. verfasserin aut Enthalten in Meteorology and atmospheric physics Wien [u.a.] : Springer, 1948 95(2006), 3-4 vom: 12. Sept., Seite 239-253 (DE-627)25463091X (DE-600)1462145-9 1436-5065 nnns volume:95 year:2006 number:3-4 day:12 month:09 pages:239-253 https://dx.doi.org/10.1007/s00703-006-0206-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE AR 95 2006 3-4 12 09 239-253 |
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10.1007/s00703-006-0206-7 doi (DE-627)SPR007306695 (SPR)s00703-006-0206-7-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Vidyunmala, V. verfasserin aut The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model 2006 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Summary The factors that control the strength of the ITCZ (Inter Tropical Convergence Zone) in an aquaplanet GCM (General Circulation Model) have been investigated. The strength of the equatorial ITCZ was found to increase rapidly with increase in meridional gradient of SST. On the other hand, the strength of the off-equatorial ITCZ does not increase rapidly with increase in meridional gradient of SST. This unusual difference in behavior between off-equatorial and equatorial ITCZ has been interpreted with a diagnostic model. The diagnostic model is based on budgets of moisture and dry static energy in the ITCZ. The diagnostic model indicates that the variations in the strength of the ITCZ are related to changes in the net energy convergence and vertical moist static stability. It was found that the net energy convergence in the off-equatorial ITCZ increases much less rapidly with meridional SST gradient than the equatorial counterpart. This difference in the behavior of net energy convergence is related to the surface wind speed which in the off-equatorial ITCZ simulation is largely insensitive to changes in the meridional SST gradient. Thus the primary difference between the equatorial and off-equatorial ITCZ is on account of the fact that wind speeds were lower in the former (on account of the constraint that zonal wind has to be zero at the equator). The impact of increasing the SST maximum on the strength of the ITCZ has also been studied. It was found that the strength of ITCZ increases with an increase in SST maximum. This increase in the strength of the ITCZ with the maximum SST is governed by the increase in boundary layer specific humidity and its impact on vertical moist static stability. Surface Wind Speed (dpeaa)DE-He213 Hadley Circulation (dpeaa)DE-He213 Moisture Convergence (dpeaa)DE-He213 Diagnostic Model (dpeaa)DE-He213 Meridional Gradient (dpeaa)DE-He213 Nanjundiah, R. S. verfasserin aut Srinivasan, J. verfasserin aut Enthalten in Meteorology and atmospheric physics Wien [u.a.] : Springer, 1948 95(2006), 3-4 vom: 12. Sept., Seite 239-253 (DE-627)25463091X (DE-600)1462145-9 1436-5065 nnns volume:95 year:2006 number:3-4 day:12 month:09 pages:239-253 https://dx.doi.org/10.1007/s00703-006-0206-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 ASE AR 95 2006 3-4 12 09 239-253 |
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English |
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Enthalten in Meteorology and atmospheric physics 95(2006), 3-4 vom: 12. Sept., Seite 239-253 volume:95 year:2006 number:3-4 day:12 month:09 pages:239-253 |
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Enthalten in Meteorology and atmospheric physics 95(2006), 3-4 vom: 12. Sept., Seite 239-253 volume:95 year:2006 number:3-4 day:12 month:09 pages:239-253 |
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Surface Wind Speed Hadley Circulation Moisture Convergence Diagnostic Model Meridional Gradient |
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Meteorology and atmospheric physics |
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Vidyunmala, V. @@aut@@ Nanjundiah, R. S. @@aut@@ Srinivasan, J. @@aut@@ |
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2006-09-12T00:00:00Z |
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The strength of the equatorial ITCZ was found to increase rapidly with increase in meridional gradient of SST. On the other hand, the strength of the off-equatorial ITCZ does not increase rapidly with increase in meridional gradient of SST. This unusual difference in behavior between off-equatorial and equatorial ITCZ has been interpreted with a diagnostic model. The diagnostic model is based on budgets of moisture and dry static energy in the ITCZ. The diagnostic model indicates that the variations in the strength of the ITCZ are related to changes in the net energy convergence and vertical moist static stability. It was found that the net energy convergence in the off-equatorial ITCZ increases much less rapidly with meridional SST gradient than the equatorial counterpart. This difference in the behavior of net energy convergence is related to the surface wind speed which in the off-equatorial ITCZ simulation is largely insensitive to changes in the meridional SST gradient. Thus the primary difference between the equatorial and off-equatorial ITCZ is on account of the fact that wind speeds were lower in the former (on account of the constraint that zonal wind has to be zero at the equator). The impact of increasing the SST maximum on the strength of the ITCZ has also been studied. It was found that the strength of ITCZ increases with an increase in SST maximum. This increase in the strength of the ITCZ with the maximum SST is governed by the increase in boundary layer specific humidity and its impact on vertical moist static stability.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Surface Wind Speed</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Hadley Circulation</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Moisture Convergence</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Diagnostic Model</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Meridional Gradient</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nanjundiah, R. 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Vidyunmala, V. |
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Vidyunmala, V. ddc 550 bkl 38.80 misc Surface Wind Speed misc Hadley Circulation misc Moisture Convergence misc Diagnostic Model misc Meridional Gradient The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model |
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550 ASE 38.80 bkl The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model Surface Wind Speed (dpeaa)DE-He213 Hadley Circulation (dpeaa)DE-He213 Moisture Convergence (dpeaa)DE-He213 Diagnostic Model (dpeaa)DE-He213 Meridional Gradient (dpeaa)DE-He213 |
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ddc 550 bkl 38.80 misc Surface Wind Speed misc Hadley Circulation misc Moisture Convergence misc Diagnostic Model misc Meridional Gradient |
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The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model |
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The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model |
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Vidyunmala, V. |
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Vidyunmala, V. Nanjundiah, R. S. Srinivasan, J. |
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effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial itcz in an aquaplanet general circulation model |
| title_auth |
The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model |
| abstract |
Summary The factors that control the strength of the ITCZ (Inter Tropical Convergence Zone) in an aquaplanet GCM (General Circulation Model) have been investigated. The strength of the equatorial ITCZ was found to increase rapidly with increase in meridional gradient of SST. On the other hand, the strength of the off-equatorial ITCZ does not increase rapidly with increase in meridional gradient of SST. This unusual difference in behavior between off-equatorial and equatorial ITCZ has been interpreted with a diagnostic model. The diagnostic model is based on budgets of moisture and dry static energy in the ITCZ. The diagnostic model indicates that the variations in the strength of the ITCZ are related to changes in the net energy convergence and vertical moist static stability. It was found that the net energy convergence in the off-equatorial ITCZ increases much less rapidly with meridional SST gradient than the equatorial counterpart. This difference in the behavior of net energy convergence is related to the surface wind speed which in the off-equatorial ITCZ simulation is largely insensitive to changes in the meridional SST gradient. Thus the primary difference between the equatorial and off-equatorial ITCZ is on account of the fact that wind speeds were lower in the former (on account of the constraint that zonal wind has to be zero at the equator). The impact of increasing the SST maximum on the strength of the ITCZ has also been studied. It was found that the strength of ITCZ increases with an increase in SST maximum. This increase in the strength of the ITCZ with the maximum SST is governed by the increase in boundary layer specific humidity and its impact on vertical moist static stability. |
| abstractGer |
Summary The factors that control the strength of the ITCZ (Inter Tropical Convergence Zone) in an aquaplanet GCM (General Circulation Model) have been investigated. The strength of the equatorial ITCZ was found to increase rapidly with increase in meridional gradient of SST. On the other hand, the strength of the off-equatorial ITCZ does not increase rapidly with increase in meridional gradient of SST. This unusual difference in behavior between off-equatorial and equatorial ITCZ has been interpreted with a diagnostic model. The diagnostic model is based on budgets of moisture and dry static energy in the ITCZ. The diagnostic model indicates that the variations in the strength of the ITCZ are related to changes in the net energy convergence and vertical moist static stability. It was found that the net energy convergence in the off-equatorial ITCZ increases much less rapidly with meridional SST gradient than the equatorial counterpart. This difference in the behavior of net energy convergence is related to the surface wind speed which in the off-equatorial ITCZ simulation is largely insensitive to changes in the meridional SST gradient. Thus the primary difference between the equatorial and off-equatorial ITCZ is on account of the fact that wind speeds were lower in the former (on account of the constraint that zonal wind has to be zero at the equator). The impact of increasing the SST maximum on the strength of the ITCZ has also been studied. It was found that the strength of ITCZ increases with an increase in SST maximum. This increase in the strength of the ITCZ with the maximum SST is governed by the increase in boundary layer specific humidity and its impact on vertical moist static stability. |
| abstract_unstemmed |
Summary The factors that control the strength of the ITCZ (Inter Tropical Convergence Zone) in an aquaplanet GCM (General Circulation Model) have been investigated. The strength of the equatorial ITCZ was found to increase rapidly with increase in meridional gradient of SST. On the other hand, the strength of the off-equatorial ITCZ does not increase rapidly with increase in meridional gradient of SST. This unusual difference in behavior between off-equatorial and equatorial ITCZ has been interpreted with a diagnostic model. The diagnostic model is based on budgets of moisture and dry static energy in the ITCZ. The diagnostic model indicates that the variations in the strength of the ITCZ are related to changes in the net energy convergence and vertical moist static stability. It was found that the net energy convergence in the off-equatorial ITCZ increases much less rapidly with meridional SST gradient than the equatorial counterpart. This difference in the behavior of net energy convergence is related to the surface wind speed which in the off-equatorial ITCZ simulation is largely insensitive to changes in the meridional SST gradient. Thus the primary difference between the equatorial and off-equatorial ITCZ is on account of the fact that wind speeds were lower in the former (on account of the constraint that zonal wind has to be zero at the equator). The impact of increasing the SST maximum on the strength of the ITCZ has also been studied. It was found that the strength of ITCZ increases with an increase in SST maximum. This increase in the strength of the ITCZ with the maximum SST is governed by the increase in boundary layer specific humidity and its impact on vertical moist static stability. |
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| container_issue |
3-4 |
| title_short |
The effect of variation in sea-surface temperature and its meridional gradient on the equatorial and off-equatorial ITCZ in an Aquaplanet General Circulation model |
| url |
https://dx.doi.org/10.1007/s00703-006-0206-7 |
| remote_bool |
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| author2 |
Nanjundiah, R. S. Srinivasan, J. |
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Nanjundiah, R. S. Srinivasan, J. |
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| doi_str |
10.1007/s00703-006-0206-7 |
| up_date |
2024-07-04T02:45:59.701Z |
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1803614850596732928 |
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| score |
7.402793 |