Map of the bays, harbors, and rivers around New York : showing the channels, soundings, lighthouses, buoys &c., and the complete topography of the surrounding country : including Hempstead, Sandy-Hook, South-Amboy, Newark, Yonkers, N. Rochelle & Glen Cove /

Relief shown by hachures. Depths shown by contours and soundings.

On the effect of Arabian Sea and Indian Ocean sea surface temperature anomaly on the monsoon rainfall of south-east of Iran

Southeast region of the country has hot and dry weather which causes to happen heavy rainfall in short time period of warm seasons and to occur river flooding. These precipitations are influenced by monsoon system of India ocean. In these thesis, It was tried to evaluate the relation between thermal anomaly of sea surface in India ocean and Arab sea which effects on southeast monsoon precipitations of Iran, For evaluation of this happening in southeast, data were collected from 7 synoptic observation stations of Bandar Abbas, Minab, Kerman , Bam, Chabahar, Iranshahr, Zahedan and 17 rain gauge stations during June to September of each year from 1980 to 2010. Rainy days were determine and then some information about synoptic circulation models, maps of average pressure of sea surface, geopotential height of 700hP surface, geopotential height of 500hP surface, temperature of 850 hPa surface, humidity of 700 hPa surface, vertical velocity of 700 hPa surface, vertical velocity of 500 hP and humidity of 2 meters height for 6 systems were extracted from NCEP/NCAR website for evaluation. By evaluation of these systems it was determined that the monsoon low pressure system tab brings needed humidity of these precipitations to this region from India ocean and Arab sea with a vast circulation. It is seen that warm air pool locates on Iran and cold air pool locates on west of India at 800 hPa surface. In a rainy day this warm air transfers to high latitudes and influences the temperature trough of southeast cold air pool of the country. In the middle surfaces of 700 and 500 hPa, the connection between low height system above India and low height system above the higher latitudes causes the low height system above India to be strength and developed. By evaluation of humidity at 2 meters height and 700 hPa surface we observe that humidity Increases in the southeast region. With penetrating of the low height system of India above the 700 and 500 hPa surfaces of southeast of Iran, the value of negative omega (Rising vertical velocity) is increased. In the second pace, it was shown the evaluation of how the correlation between sea surface temperature anomaly in India Ocean and Arab sea influences southeast monsoon precipitation of Iran. For this purpose the data of water surface temperature anomaly of Arab sea and India ocean, the data of precipitation anomaly of 7 synoptic stations , mentioned above, and correlation coefficient among the data of precipitation anomaly and water surface temperature anomaly of Arab Sea, east and west of India ocean were calculated. In conclusion it was shown that the maximum correlation coefficient of precipitation anomaly had belonged to India Ocean in June and no meaningful correlation was resulted in July among precipitation anomaly and sea surface temperature anomaly for three regions, which were evaluated.

Plat of proposed carriage road and other improvements south of the President's House : agreeably to plan of A.J. Downing for improvement of said roads & grounds /

"3d day of October 1854."

Map of Jackson City opposite the city of Washington at the south end of the Potomac Free Bridge.

Shows proposed town of Jackson City in Alexandria County D.C.

South-Carolina and parts adjacent, shewing the movements of the American and British armies.

Shows troop movements during 1781.

[Plat of land grant survey in South Carolina, accompanied by deed of grant] /

Pen-and-ink.

Plan of 59 different tracts of land (of 1000 acres each) containing in the whole 59,000 acres : situate on different waters of south Edisto River, except seven tracts (or 7000 acres) are lying on the waters of north Edisto River in the District of Orangeburgh, State of South Carolina /

Pen-and-ink and watercolor.

Plan von dem Haven und der Gegend von Charles Town in South Carolina ... Sept. 1782

Scale ca. 1:250,000.

A sketch of the operations before Charlestown, the capital of South Carolina.

Scale ca. 1:11,800.

Map of 1st. distrt. Campbell Co. Georgia : south of the Cherokee boundy. line /

Shows local topography, roads, and names of some residents.

Spratly Islands in the South China Sea.

"1401212-15 State (INR)."

Rural change south of the river Bride in counties Cork and Waterford: the surveyors' evidence 1716–1851

Estate studies in Irish historical geography have been often designed to confirm or contrast local trends of development with those previously identified at the regional or sub-regional level. To date, little attention has been awarded to estate maps in studies of rural landscape change. It is a theme of this paper that the results yielded from a careful study of such estate maps can throw light on the results of the activities of the majority of estate residents. In this regard, it is fortunate that at Lismore surveys of the estate in 1716–17 and 1773–4 have survived, and a nineteenth century dimension is added by an analysis of the Valuation Office maps for 1851. This work is focused on a study of critical indicators of change, notably leasing arrangements, farm size, rate and type of enclosure, infrastructural development and settlement growth. These changes are reviewed within the framework of the dialectic that developed between landlord or landlord-inspired management policies and the forces released locally by the vast bulk of the population. Broadly this analysis indicates some of the potential rewards which may be secured by detailed scrutiny of estate maps in conjunction with other estate records.

Southeast Asia

Southeast Asia occupies the mainland area east of India and south of China, as well as the archipelago between the mainland and Australia, west of the Pacific Ocean. The region is self-identified by its geographic proximity, although cultural commonalities across the region occur mostly at the level of consensus gentium rather than as an overarching mode of regional distinction. Its peoples derive from a broad East Asian racial grouping, dividing primarily along linguistic lines into four families of languages. These linguistic families thereafter quickly devolve into hundreds of ethnic groups, many of which have been bound together in postcolonial states that, to various degrees, comply or otherwise with precolonial polities. While some states have a strong sense of coherent national identity, others have had to consciously construct such an identity, with varying degrees of success and not a little resistance.