Search Results
1. Shiyatov - Altyn-Beshik - JUTU - ITRDB KYRG008
Shiyatov, S. Earliest Year: 530 cal yr BP (1420 AD) * Most Recent Year: -37 cal yr BP (1987
AD) * Location Bounds - North: 40.2 * South: 40.2 * East:72.5833 * West: 72.5833 *
Past global climate changes had strong regional expression. To elucidate their spatio-temporal
pattern, we reconstructed past temperatures for seven continental-scale regions during the past
one to two millennia. The most coherent feature in nearly all of the regional temperature
reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multidecadal to centennial scales, temperature variability shows distinctly different regional patterns,
with more similarity within each hemisphere than between them. There were no globally
synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period
or Little Ice Age, but all reconstructions show generally cold conditions between ad 1580 and
1880, punctuated in some regions by warm decades during the eighteenth century. The transition
to these colder conditions occurred earlier in the Arctic, Europe and Asia than in North America or
the Southern Hemisphere regions. Recent warming rev...
2. Shiyatov - Kursala Ridge - JUTU - ITRDB KYRG009
Shiyatov, S. Earliest Year: 931 cal yr BP (1019 AD) * Most Recent Year: -37 cal yr BP (1987
AD) * Location Bounds - North: 39.9167 * South: 39.9167 *East: 71.4667 * West: 71.4667 *
Past global climate changes had strong regional expression. To elucidate their spatio-temporal
pattern, we reconstructed past temperatures for seven continental-scale regions during the past
one to two millennia. The most coherent feature in nearly all of the regional temperature
reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multidecadal to centennial scales, temperature variability shows distinctly different regional patterns,
with more similarity within each hemisphere than between them. There were no globally
synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period
or Little Ice Age, but all reconstructions show generally cold conditions between ad 1580 and
1880, punctuated in some regions by warm decades during the eighteenth century. The transition
to these colder conditions occurred earlier in the Arctic, Europe and Asia than in North America or
the Southern Hemisphere regions. Recent warming rev...
3. Shiyatov - Marble Quarry - JUTU - ITRDB KYRG010
Shiyatov, S. Earliest Year: 523 cal yr BP (1427 AD) * Most Recent Year: -37 cal yr BP (1987
AD) * Location Bounds - North: 40.1667 * South: 40.1667 *East: 72.6167 * West: 72.6167 *
Past global climate changes had strong regional expression. To elucidate their spatio-temporal
pattern, we reconstructed past temperatures for seven continental-scale regions during the past
one to two millennia. The most coherent feature in nearly all of the regional temperature
reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multidecadal to centennial scales, temperature variability shows distinctly different regional patterns,
with more similarity within each hemisphere than between them. There were no globally
synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period
or Little Ice Age, but all reconstructions show generally cold conditions between ad 1580 and
1880, punctuated in some regions by warm decades during the eighteenth century. The transition
to these colder conditions occurred earlier in the Arctic, Europe and Asia than in North America or
the Southern Hemisphere regions. Recent warming rev...
4. Shiyatov - Sheveli Canyon - JUTU - ITRDB KYRG011
Shiyatov, S. Earliest Year: 1256 cal yr BP (694 AD) * Most Recent Year: -37 cal yr BP (1987
AD) * Location Bounds - North: 39.8333 * South: 39.8333 *East: 71.5 * West: 71.5 *
Past global climate changes had strong regional expression. To elucidate their spatio-temporal
pattern, we reconstructed past temperatures for seven continental-scale regions during the past
one to two millennia. The most coherent feature in nearly all of the regional temperature
reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multidecadal to centennial scales, temperature variability shows distinctly different regional patterns,
with more similarity within each hemisphere than between them. There were no globally
synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period
or Little Ice Age, but all reconstructions show generally cold conditions between ad 1580 and
1880, punctuated in some regions by warm decades during the eighteenth century. The transition
to these colder conditions occurred earlier in the Arctic, Europe and Asia than in North America or
the Southern Hemisphere regions. Recent warming rev