Aviation intermediate maintenance manual : target acquisition designation sight (TADS) assembly AN/ASQ-170, AH-64A attack helicopter.

"30 April 1985."

Field and depot maintenance manual : receivers, radio R-1041/ARN and R-1041A/ARN.

"18 November 1963."

DS, GS, and depot maintenance repair parts and special tools lists : receivers, radio R-1041/ARN, R-1041A/ARN, and R-1041B/ARN.

Includes indexes.

Operator and organizational maintenance manual : receivers, radio R-1041/ARN and R-1041A/ARN.

"13 May 1963."

Field and depot maintenance manual : receivers, radio R-1041/ARN and R-1041A/ARN.

"18 November 1963."

Organizational, direct support, and general support maintenance repair parts and special tools lists (including depot maintenance repair parts and special tools) for signal generator AN/URM-170 (NSN 6625-00-883-3256).

Includes index.

Quartets for stringed instruments: K.80, 155, 156, 157, 158, 159, 160, 168, 170, 171, 172, 173.

G major, K.80.--D major, K.155.--G major, K.156.--C major, K.157.--F major, K.158.--B♭ major, K.159.--E♭ major, K.160.--F major, K.168.--A major, K.169.--C major, K.170.--E♭ major, K.171.--B♭ major, K.172.--D minor, K.173.

Minnesota's double-barrelled implied consent law : a 1983 update of "Analytical study of the legal and operational aspects of the Minnesota law entitled ʻChemical test for intoxication,"̓ DOT/HS-806-170 (Robert H. Reeder) /

"December 1983."

Particle size of Saharan dust in the Atlantic Ocean, from October 2012 to November 2013

Mineral dust has a large impact on regional and global climate, depending on its particle size. Especially in the Atlantic Ocean downwind of the Sahara, the largest dust source on earth, the effects can be substantial but are poorly understood. This study focuses on seasonal and spatial variations in particle size of Saharan dust deposition across the Atlantic Ocean, using an array of submarine sediment traps moored along a transect at 12° N. We show that the particle size decreases downwind with increased distance from the Saharan source, due to higher gravitational settling velocities of coarse particles in the atmosphere. Modal grain sizes vary between 4 and 33 µm throughout the different seasons and at five locations along the transect. This is much coarser than previously suggested and incorporated into climate models. In addition, seasonal changes are prominent, with coarser dust in summer, and finer dust in winter and spring. Such seasonal changes are caused by transport at higher altitudes and at greater wind velocities during summer than in winter. Also the latitudinal migration of the dust cloud, associated with the Intertropical Convergence Zone, causes seasonal differences in deposition as the summer dust cloud is located more to the north, and more directly above the sampled transect. Furthermore, increased precipitation and more frequent dust storms in summer coincide with coarser dust deposition. Our findings contribute to understanding Saharan dust transport and deposition relevant for the interpretation of sedimentary records for climate reconstructions, as well as for global and regional models for improved prediction of future climate.