“Out of These Ghettos, People Who Would Fight”

Author(s):  
Roberta Gold

This chapter examines the rent strikes that erupted in Harlem and other ghettos in the 1960s. Ideologically, the rent strikes blur the line between civil rights liberalism and Black Power. Rent strikers renounced the liberal integrationist vision—moving out of the ghetto—that had animated the previous decade's black housing struggles. Instead they sought to improve conditions and build power within the segregated neighborhoods where they, like most African Americans, actually lived. This chapter considers the rent rebellion launched by ghetto residents, drawing inspiration from the burgeoning civil rights movement and support from New York's longtime tenant advocates. It shows that this rent rebellion won modest material improvements and contributed to a growing movement for community power in the ghettos. One of the strikes' main achievements was to galvanize tenants throughout New York City at a critical moment in the long-term fight over rent control. The chapter also discusses issues of gender and race in the Harlem rent strikes.

2012 ◽  
Vol 25 (19) ◽  
pp. 6721-6742 ◽  
Author(s):  
Richard Seager ◽  
Neil Pederson ◽  
Yochanan Kushnir ◽  
Jennifer Nakamura ◽  
Stephanie Jurburg

Abstract The precipitation history over the last century in the Catskill Mountains region that supplies water to New York City is studied. A severe drought occurred in the early to mid-1960s followed by a wet period that continues. Interannual variability of precipitation in the region is related to patterns of atmospheric circulation variability in the midlatitude east Pacific–North America–west Atlantic sector with no link to the tropics. Associated SST variations in the Atlantic are consistent with being forced by the anomalous atmospheric flow rather than being causal. In winter and spring the 1960s drought was associated with a low pressure anomaly over the midlatitude North Atlantic Ocean and northerly subsiding flow over the greater Catskills region that would likely suppress precipitation. The cold SSTs offshore during the drought are consistent with atmospheric forcing of the ocean. The subsequent wet period was associated with high pressure anomalies over the Atlantic Ocean and ascending southerly flow over eastern North America favoring increased precipitation and a strengthening of the Northern Hemisphere storm track. Neither the drought nor the subsequent pluvial are simulated in sea surface temperature–forced atmosphere GCMs. The long-term wetting is also not simulated as a response to changes in radiative forcing by coupled models. It is concluded that past precipitation variability in the region, including the drought and pluvial, were most likely caused by internal atmospheric variability. Such events are unpredictable and a drought like the 1960s one could return while the long-term wetting trend need not continue—conclusions that have implications for management of New York City’s water resources.


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