The new a-theory of time

The New A-theory of Time (TNAT) is the view, to be elaborated and defended in this article, that many times exist, and that time is real in virtue of every moment in time bearing each of the so-called A-properties: past, present and future. I argue that TNAT is at least as theoretically virtuous as mainstream views in the philosophy of time and may have some claim to being our best theory of time. I show that the properties ‘past’, ‘present’ and ‘future’ can be understood as compatible intrinsic properties. Having demonstrated that this account of the A-properties is coherent, I go on to demonstrate how TNAT can give us an account of passage, change and the truth-conditions for temporal sentences. In the final section of the article, I develop a tentative argument in favour of TNAT, though concede that we have to settle for the result that TNAT is on a par with our other theories of time. In the remainder of this opening section, my aim is to situate the current proposal as a direct response to McTaggart’s infamous argument against the reality of time

The Agricultural Outlook: 1965

The general economic picture for 1965 indicates another better-than average year for the nation as a whole. Strong advances in economic activity now underway will likely continue at least through the first half of the year. Current trends reveal no serious imbalances in the economy. Forces expected to shape demand expansion for business, consumers and the government in coming months are (1) continued uptrend in business investments, (2) favorable inventory-sales ratios, (3) further improvement in the goods and services export-import trade balance, (4) more favorable factors affecting demand for housing, schools, and facilities, (5) expanded consumer purchases of goods and services, (6) another big sales year for autos, (7) larger consumer expenditures for food, and (8) increased government purchases of goods and services

Deep western boundary current east of Abaco: mean structure and transport

To assess whether the southward deep water flow of the Atlantic meridional overturning circulation can be monitored by measuring the deep western boundary current, the structure and transport of the time-averaged deep western boundary current at 26.5N are estimated from long current meter records deployed in a series of 7 mooring deployments over 11 years from March 1986 to June 1997 east of Abaco Island in the Bahamas. Time-averaged meridional velocities for each current meter record are combined into estimates of mean velocity at 3 to 10 depths at 10 mooring locations extending eastward from the continental slope out to an offshore distance of 580 km. The mean deep western boundary current below 1000 m depth exhibits a core of strong southward velocities above 15 cm s-1 at an offshore distance of about 55 km and extends out to an offshore distance of about 160 km with an estimated total southward transport of 34.6 Sv. We estimate the error in this time-averaged transport to be 3.7 Sv due to uncertainties in the mean velocities due to temporal variability and up to 4 Sv due to the choice of methods to integrate spatially the time-averaged velocities across the section. Offshore from 160 km out to at least 580 km, there is broad, slow northward flow that recirculates deep water northward. While the mooring array is not sufficient to accurately measure the northward recirculation, a simple spatial average of the time-averaged currents indicates a northward recirculation of about 13 Sv in this offshore region. Daily estimates of the deep western boundary current from two arrays with reasonably complete coverage of the deep western boundary current suggest that the instantaneous boundary current has a width of about 100 km, naturally narrower than the mean boundary current. Daily southward transports vary between 5 and 75 Sv but the array does not fully resolve the boundary current during offshore meander events that occur about 20% of the time. We conclude that it is problematic to monitor the net southward flow of the Atlantic meridional overturning circulation with boundary current measurements at 26.5N because the narrow deep western boundary current transport has substantially larger transport than the net southward flow and the offshore northward recirculation is broad and diffuse so that accurate estimates of the recirculation would require an extensive array of moored instruments