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The design integrations are performed towards the Geophysical Water Character Research (GFDL) Atmospheric Model adaptation dos

Sunday, October 2nd 2022.

The design integrations are performed towards the Geophysical Water Character Research (GFDL) Atmospheric Model adaptation dos

1) Design operates put

1 (Delworth mais aussi al. 2006) presenting a limited-volume dynamical key (Lin 2004) that have a lateral quality of about 2° latitude and you may twenty four straight membership. The brand new atmospheric model was coupled in order to an excellent slab sea having spatially uniform breadth. Five ensemble members having given sea deepness from 2.cuatro, six, 12, 24, and 50 yards are analyzed within research. The fresh design is actually pushed of the seasonally differing insolation which have zero eccentricity and ° obliquity, and is focus on to own two decades, enough to converge to your a stable climatology. The newest design climatology are extracted from the past five years regarding the new integrations.

2) Show

The seasonal migration of the ITCZ off the equator has a larger amplitude for shallower ocean depths (Fig. 8) and PPenny reaches as far as 21° in the 2.4-m slab depth run as compared to 3° in the 50-m slab depth run. This behavior is expected because the adjustment time scale of a 50-m-deep ocean to solar heating is on the order of one year (Donohoe 2011) as compared to weeks for 2.4-m-deep ocean. Thus, the SSTs barely adjust to the seasonally varying insolation in the 50-m run while the maximum SST moves seasonally with the insolation in the 2.4-m run.

(top) Regular range of rain centroid and you may atmospheric temperatures transport along the equator on slab water aquaplanet simulations with each simulation (water breadth) provided by an alternative colour. The newest regular assortment are twice this new amplitude of one’s annual harmonic of each changeable in addition to hill of your line ‘s the regression coefficient of your monthly data. The latest black colored asterisks is the month-to-month observations and also the good black range ‘s the regular listing of new findings. (bottom) Since within better, but for precipitation centroid and you can warm SST gradient.

(top) Seasonal directory of precipitation centroid and you can atmospheric heat transport along side equator best lesbian dating apps on slab sea aquaplanet simulations with every simulation (water breadth) given by another type of colour. The fresh new regular assortment was double the new amplitude of one’s yearly harmonic of each and every varying as well as the mountain of your range ‘s the regression coefficient of month-to-month data. The fresh black colored asterisks may be the month-to-month observations and strong black colored line ‘s the seasonal set of the latest observations. (bottom) As the during the most useful, however for precipitation centroid and you will warm SST gradient.

(top) Seasonal listing of rain centroid and you can atmospheric temperature transportation along side equator regarding the slab sea aquaplanet simulations with each simulation (ocean breadth) provided by an alternate colour. The seasonal variety is twice the new amplitude of annual harmonic each and every variable as well as the mountain of your own line is the regression coefficient of your own month-to-month research. The brand new black asterisks would be the month-to-month findings together with strong black line is the regular set of the fresh findings. (bottom) Because the at the most readily useful, but for rain centroid and you can warm SST gradient.

The seasonal amplitude of AHTEQ also decreases with increasing ocean depth, from 11.6 PW in the 2.4-m run to 0.5 PW in the 50-m run. In the shallow ocean run, the SSTs respond rapidly to the seasonally varying insolation, heating up over the summer hemisphere and subsequently fluxing energy upward (via turbulent and longwave fluxes) to the adjacent atmosphere to drive seasonal variations in AHTEQ; in the 2.4-m run ?SHF? is nearly in phase with the insolation (11-day lag) and has a seasonal amplitude of 11.6 PW. In contrast, the solar heating of the ocean makes a minimal impact on ocean temperatures in the deep ocean runs due to the large heat capacity of the ocean. In fact, SWABS is the only source of seasonal atmospheric heating in the 50-m run and the atmosphere loses energy to the ocean during the warm season; in the 50-m run ?SHF? is nearly antiphased with the insolation (192-day lag) and has a seasonal amplitude of 3.7 PW.

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